ALBERT

Description / Table of Contents: PREFACE The Lower Triassic Buntsandstein in Middle Europe which originated in mainly continental fluvla] environment in the Mid-European Triassic Basin is a famous terrestrial red bed sequence that is discussed in the geological literature since more than 200 years. Much of the earlier work had been devoted to stratigraphical, palaeogeographical and petrographical problemsof the Buntsandstein. The sedimentological analysis and deposltional modelling in the German-type facies, however, is the youngest branch of Buntsandstein investigation and started only a few decades ago. During the last ten years when I began to concentrate on the interpretation of the genesis of the Buntsandstein, much work has been carried out and has already been documented in numerous papers that focussed on various aspects of sedimentology, particularly on reconstruction of fluvial and aeolian depositional mechanisms, significance of palaeosols, importance of fluvial conglomerates, palaeoecology of the fossils, interdisciplinary sedimentology, diagenesis of heavy minerals and origin of the red colour. A summary of the present knowledge in the western part of the German Basin is given in a compilation of regional articles together with general discussions and comparative contributions and especially with an extensive colour photographic documentation in an earlier book (reference on p. 12). In the last few years when more and more material became available not only from the Buntsandstein s. str. (Lower Triassic Scythian) in the Mid-European Triassic Basin, but also from correlative sequences in adjoining areas and even older or younger series of similar facies and origin, it became more and more evident that a synthesis of the state of the art would be necessary, if not inevitably for outlining the general frame and illustrating the diversification of facies associations in numerous temporal and spatial scales. That is why I decided to edit an international proceedings volume on the Buntsandstein which is to compile contributions from many regions and different stratigraphic units with emphasis on various aspects of fluvia] sedi~ntation, but stressing also the importance of the distribution of associated environments such as aeolian dunes and calcrete palaeosols. In spite of my own enthusiasm for the Buntsandstein continental red bed formation (the Lower Triassic red rocks seem to have a very special flavour for being so attractive for me) and regardless of the expansion of my investigations from my original Eife] area (where I learnt how to assess the facies assoCiations in terms of depositional modelling and where I collected an enormous amount of data that served as a valuable base for the production of various case studies which were published during the last years) to several other regions, it was without any doubt that it would not be possible for me alone to finish such an overregional proceedings book within a reasonable time, but that I had to beg various colleagues for their collaboration by writing papers on the Buntsandstein in their investigated areas for this volume. Although the response to my first and second circulars soon showed that it would not be possible to publish a compilation of articles from almost all the studied regions, formations and aspects within a reasonable time with avoiding too much delay of appearance for early contributors, I am very happy that finally many colleagues provided me with papers from almost all the countries in Europe where Buntsandstein is cropping out at the surface. In spite of the tremendous editorial work which was necessary to polish the English, to improve the contents of text and drawings and to put the sequence of papers into a general stream line, I would like to thank all my colleagues who contributed to this volume for their support of the project and particularly for their understanding of my editorial task, especially in case of my frequently serious intervention into their early manuscripts and illustrations. Looking for a publisher in the early stages of planning the volume, I found immediately support by Dr. W. Engel (Department of Geological Sciences of the Springer- Verlag) who generously offered me to take the book into the newly founded series "Lecture Notes in Earth Sciences". From the beginning of organization, writing and editing, I appreciated very much the close cooperation with Dr. Engel who always had an ear for my problems and gave me the necessary freedom to finish the volume along the lines of my intention. Although the preparation of the camera-ready manuscript leaves nearly all the work and responsibility with the author, I am especially grateful to Dr. Engel for his guarantee of almost immediate publication after receipt of the final manuscript which allowed me to polish and incorporate latest ideas up to the very terminal moment. Writing on a subject like the Buntsandstein which has proven to be considerably diversified in terms of sedimentary processes and depositional mechanisms, it became soon apparent that a full discussion along my original intention would easily end up with several thousands of pages in size and would consume much more than a few years. Having already rePeatedly experienced in the past that during course of incorporation of nearly all the relevant literature, the reference l i s t of the final paper is often longer than the whole first draft of the article after one or two years collection of data and ideas, there was no other way than to decide to keep the bibliography short. In order to restrict the book to an economical frame and not to frighten the readership to death, but especially to avoid drowning of the red line through the volume, many contributions had to be written as summary presentations without detailed discussion of the literature. Speaking particularly for the articles that have been written by myself either alone or together with friends, I can assure that this is by no means the result of proud neglectance of other works, but only the necessity of streamlining of the book, and that much of the detailed discussion of comparative examples from the literature has to be done in subsequent special papers. It is impossible to acRnowledge all the people that helped me to arrive at the present goal. Special merits, however, deserve those who stimulated my interest for the Buntsandstein. I am especially indebted to Prof. Dr. G. Fuchs (Landessammlungen fur Naturkunde, Karlsruhe) who proposed me ten years ago to work on the Eifel Buntsandstein for my M.Sc. Thesis, and who later supervised together with Prof. Dr. W. Dachroth (Department of Geology and Palaeontology, University of Heidelberg) the preparation of my Ph.D. Thesis. The good luck of the former to choose the Eifel for me as a starting region (which later proved to have a key position for approaching the evolution of fluvial sedimentation in many other Buntsandstein areas), and the earlier investigations of the latter (although largely unpublished and even only briefly touched in his contribution to this volume) triggered my love of the Buntsandstein which has reached a preliminary climax with the present book. It is my pleasure to dedicate this volume to my two former supervisors with very many thanks for their support and in honour of their merit to have lighted the fire. It is my sincere wish to acknowledge again all the people who contributed with articles to this volume for their help to prepare this summary of the state of the art of Buntsandstein fluvial sedimento]og~y. I also want to sincerely thank all friends and colleagues who supplied ideas and facts in oral or written form and who guided me in the field during course of my comparative investigations that helped me considerably in proceeding with the interpretation of the Buntsandstein. Thanks are also due to Helmut Mader (my father) and Martha Herrmann (my aunt) for their support. I am further indebted to those who have been involved in the various technical aspects of the preparation of the manuscript from the beginning of word processor typesetting of the text and reprography of the illustrations to the final printing. I do hope that the compilation of articles on fluvial aspects of the Buntsandstein in this book will stimulate the interest of many people in the topic of sedimentological modelling of terrestrial red bed sequences and will internationally highlight the position of the Buntsandstein as an extraordinarily attractive case history of fluvial deposition.

Description / Table of Contents: INTRODUCTION Sediments are increasingly recognized as both a carrier and a possible source of contaminants in aquatic systems, and these materials may also affect groundwater quality and agricultural products when disposed on land. Contaminants are not necessarily fixed permanently by the sediment, but may be recycled via biological and chemical agents both within the sedimentary compartment and the water column. Bioaccumulation and food chain transfer may be strongly affected by sediment-associated proportions of pollutants. Benthic organisms, in particular, have direct contact with sediment, and the contaminant level in the sediment may have greater impact on their survival than do aqueous concentrations. Following the findings of positive correlations between liver lesions in English Sole and concentrations of certain aromatic hydrocarbons in Puget Sound (Washington) sediment, it can be suspected that such substrates may also be responsible for a host of other serious and presently unrecognized changes at both the organismal and ecosystem levels (Malins et al., 1984). Modern research on particle-bound contaminants probably originated with the idea that sediments reflect the biological, chemical and physical conditions in a water body (Züllig, 1956). Based on this concept the historical evolution of limnological parameters could be traced back from the study of vertical sediment profiles. In fact, already early in this century Nipkow (1920) suggested that the alternative sequence of layers in a sediment core from Lake Zürich might be related to variations in the trophic status of the lake system. During the following decades of limnological research on eutrophication problems sediment aspects were playing only a marginal role, until it was recognized that recycling from bottom deposits can be a significant factor in the nutrient budget of an aquatic system. Similarly, in the next global environmental issue, the acidification of inland waters sediment-related research only became gradually involved. Here too, it is now accepted that particle-interactions can affect aquatic ecosystems, e.g. by enhancing the mobility of toxic metals. In contrast to the eutrophication and acidification problems, research on toxic chemicals has included sediments aspects from its beginning: Artificial radionuclides in the Columbia and Clinch Rivers in the early sixties (Sayre et al., 1963); in the late sixties heavy metals in the Rhine River system (De Groot, 1966) and methyl mercury (Jensen & Jerne- 16v, 1967) at Minamata Bay in Japan, in Swedish lakes, in Alpine Lakes, Laurentian Great Lakes and in the Wabigoon River system in Canada; organochlorine insecticides and PCBs in Lakes St. Clair and Erie during the seventies (Frank et al., 1977); chlorobenzenes and TCDDs in the Niagara River system and Lake Ontario in the early eighties (Oliver & Nicol, 1982; Smith et al., 1983). In the present lecture notes, following the description of priority pollutants related to sedimentary phases (Chapter 2), four aspects will be covered, which in an overlapping succession also reflect the development of knowledge in particle-associated pollutants during the past twenty-five years: - the identification, surveillance, monitoring and control of sources and distribution of pollutants (Chapter 3); - the evaluation of solid/solution relations of contaminants in surface waters (Chapter 4); - the study of in-situ processes and mechanisms in pollutant transfer in various compartments of the aquatic ecosystems (Chapter 5);- The assessment of the envlroD-mental impact of particle-bound contaminants, i.e. the development of sediment quality criteria (Chapter 6). A final chapter will focus on practical aspects with contaminated sediments. Available technologies will be described as well as future perspectives for the management of dredged materials. Here too, validity of remedial measures can only be assessed by integrated, multidisciplinary research. In the view of the growing information on the present subject and owing to the limitations in the framework of this monography, the reader is referred to additional selected bibliography, which is attached at the end of this Chapter i. Additional information on the more recent publications on contaminated sediments is given in the annual review volume of the Journal of the Water Pollution Control Federation, June edition.

Description / Table of Contents: The study of calcareous bedding rhythms has become an important field in Geology. Often these bedding rhythms are simply interpreted as representations of primary climatic cycles without showing the effects of any appreciable diagenetic overprinting. This study, however, deals predominantly with the diagenetic processes which are usually large and affect both the amplitude and rhythm of carbonate oscillations. The purpose of this textbook is two fold. First, it intends to provide a better understanding of the processes of diagenetic bedding. Secondly, this new approach allows one to quantify and to understand diagenesis in terms of mass exchanges. This is possible through the development of methods which combine chemical data with compaction measurements. These methods can be also used independent of the marl-limestone alternation problem.

Description / Table of Contents: PREFACE It is increasingly necessary to develop industrial and hydraulic engineering constructions under unfavourable geological or geotechnical conditions. Furthermore, it becomes more and more important to build effectively and economically and to find optimal solutions for a long-term steady function of the constructions. This emphatically demands exhaustive information on the structural situations and engineering parameters of local site assessments by areal investigations of the sites and the petrophysical parameters in situ. This requires, however, the use of geophysical techniques. During the last two or three decades international applied geophysics has systematically developed new possibilities for site investigations for the determination of petrophysical parameters in situ as well as for observation of the system building and site. As in "New techniques in engineering", geophysical methods make it possible to develop areal models of subsurface conditions of building sites, to quantify relevant engineering parameters in situ, as well as to analyze the longterm behaviour of the buildings, which are influenced by internal or external factors. With regard to the broad spectrum of applied geophysics, there are few methods, that especially favour application in engineering and groundwater studies. These methods are distinguished by a relatively simple measuring technique and good measuring progress, e.g. the geoelectrical self-potential method, the geoelectrical resistivity method as well as a newly developed devices for geothermic measurements. There exist numerous publications, broadly scattered in the technical literature, concerning the theoretical bases and applications of these methods, but until now, there have been only a few meetings to exchange experience and results on an international level. This was the aim of the symposium "Detection of Subsurface Flow Phenomena by Self-Potential/Geoelectrical and Thermometric Methods", held in Karlsruhe from 14-18 March 1988. An outstanding part of the symposioum was represented by the results of a research project, coordinated by the University of Karlsruhe (Department of Geology and Institute of Soil and Rock Mechanics) and the Federal Waterway Engineering and Research Institute (BAW), Karlsruhe. Regarding the subject "Experiments to ascertain the relations between hydraulic potentials in the underground and the geoelectrical and thermic potentials set off by these", the research work took four years. The project was sponsered by the Volkswagen Foundation/Hannover. The goal was to develop and test objective techniques for detecting leakages in dams, locating, demarcating and designating quantitatively inhomogeneous spheres in dams with the aim of detecting damage and subsurface flow phenomena as soon as possible. The symposium consisted of a three-day lecture meeting with about 40 papers and a summarizing respectively closing roundtable discussion, a visit to the laboratories and to the in situ constructions within the area of BAW developed in the frame of the research project. This included a technical excursion to the Rhine-Staustufe Iffezheim with its very impressive waterway constructions and an excursion to the Geophysical Observatory near Schiltach (Black Forest). The Observatory belongs to the Universities of Karlsruhe and Stuttgart. Approximately 80 scientists from 15 countries participated the symposium. They were welcomed by the Rector of the University, Professor Dr. A. Kunle and the representative of the Federal Ministry of Traffic, Dr. G. Schröder. Professor Dr. H. Hötzl elucidated the scientific problems and the economical importance of the project as a speaker of the research group. The following papers dealt with the fundamental aspects of geoelectrical and thermometric measurements, with the theory of these methods, the state and developing ter~dencies concerning devices, data acquisition, processing and interpretation as well as noise effects. It became clear that the solution of the complex scientific-technical problems of waterway constructions and environmental protection requires broad, interdisciplinary cooperation and international collaboration. Thus it would be possible to minimize the personnel, temporal and economic efforts. The intended cooperation of geoscientists, engineering geologists, building engineers and representatives of other disciplines make it possible, not only to exchange experiences and results relating to international problems unsolved until now, but also to determine new guidelines with regard to the scientific organization of further investigations. Thus in order to inform all interested parties of the main topics of the symposium and to advance international cooperation in the future, the present review includes a part of the papers and reports of the excursions recommended by the participants of the meeting, which have been divided into the following topics: - Introduction to engineering-geophysical problems and attempts at their solution; - Geoelectrical self-potential measurements; - Geoelectrical resistivity measurements; - Geothermic measurements; - Case histories; - Some topics of the roundtable discussion; - Reports concerning the excursions. The editors wish to thank very much all those, who contributed to the success of the symposium and to the publication of the present report. Finally they venture the note, that the authors theirselves are responsible for the content of their papers.

Description / Table of Contents: INTRODUCTION Evaporites may form in a spectrum of environments from continental sabkha (playa) to deep basins (see Kendall 1978 a, b, Schreiber 1978, 1986, Friedman and Krumbein 1985, for review). In the last two decades, many ancient evaporite basins have been interpreted using the sabkha model and the deep desiccated basin model, the former not excluding the latter. However, growing evidence has been gathered indicating that most evaporites are formed in subaqueous environments, so that it cannot be reasonably expected that one depositional model alone will explain the entire basin fill. The chapters in this volume discuss characteristic examples of evaporite basins, mostly of moderate size. Aspects of a saline giant, the Zechstein basin of Central and NW Europe, have been considered in Volume 10 of "Lecture Notes in Earth Sciences"...

Description / Table of Contents: This volume contains the contributions which have been presented at the 5. ALFRED WEGENER-Conference , held in Göttingen, Federal Republic of Germany, 21 - 24 May 1986. This conference was the first international meeting of the IGCP Project 216 :"global biological events in earth history". The aim of the conference was, to discuss (a) the state-of-the-art in respect to the recognition of bio-events and to the analysis of their causes (b) the presentation of new data (c) the strategies which are needed for further research, carried out in the international cooperation programme of Project 216. It was intended to achieve with these discussions a more critical approach to the problems of global bio-events.

Description / Table of Contents: OPENING ADDRESS On behalf of the Local Organizing Committee, I welcome you all to the first International Workshop on GPS-techniques in surveying and geodesy held at this university. This workshop is designed to bring together experts from various countries and also scientists who carry out, analyze and interpret such measurements with those who work on instrumental and theoretical problems. The workshop focuses hereby on high-precision applications with emphasis on monitoring time-dependent phenomena such as those relevant to geodynamics as well as men-made constructions as those in civil engineering and similar fields. It is astonishing to see how, in spite of all earlier satellite work over the last two decades, GPS-methods became so fast a relevant new technology, in its proper sense, in modern geodesy and surveying besides VLBI and Satellite Laser Ranging (SLR). With the recent development of new dual-frequency receivers the role of GPS-procedures in monitoring large-scale phenomena over big distances will still expand; and the application of kinematical GPS-approaches is of utmost interest in solving high-precision problems. It is indeed fascinating to realize how GPS-methods have become in such a short time a surprisingly efficient and effective, this means : fast, precise and easy to apply, tool which is able to replace already now, after a few years of existence and with an incomplete set of a few out of the 18 satellites (of the final stage), at least partially some expensive, slow and cumbersome classical surveying methods. On the other hand, it cannot be overemphasized that GPS-procedures are still at their beginning and the full spectrum of their capabilities still has to be explored. In Europe, for example, where excellent classical surveying systems do exist the situation is quite different from the situation in other countries such as Canada or the USA. Even within Europe the application types of GPS-methods will vary; for example, in Norway the situation is quite different from central European countries. It is often forgotten, that together with GPS we will have to introduce new concepts and a new thinking in combination with other modern satellite procedures. GPS itself can resolve only a small part of the problems to be solved by modern geodesy but it will open the way to a great variety of new applications and capabilities. Modern global tectonics is just one of the new disciplines of high interest and great practical impact. I could continue in citing other similarly important new fields. GPS is, however, of special importance because it replaces old technologies and fills gaps where modern and efficient tools are most needed. Consequently, also the optimal combination of GPS-methods with new auxiliary and also classical high-precision techniques is of great importance, mainly under the european conditions outlined above. Moreover, the real-time or almost-real-time use of GPS in combination with photogrammetry, inertial geodesy, gravity gradiometry or even classical surveying is of substantial interest. It is indeed important to realize the new concepts in modern satellite and space methods and I, therefore, spoke above of a new "technology" which should be optimally developed as there is a worldwide need of such capabilities and tools. In view of the few active NAVSTAR-satellites in sky in 1988 this is perhaps not the best year for GPS-applications but the right time for a review of the experience gained until now and using it as a base for the planning of the future...

Description / Table of Contents: INTRODUCTION - WHY THIS BOOK? Why study Numerical Geology? Although geologists have dabbled in numbers since the time of Hutton and Playfair, 200 years ago (Merriam 1981e), geology until recently lagged behind other sciences in both the teaching and geological application of mathematics, statistics and computers. Geology Departments incorporating these disciplines in their undergraduate courses are still few (particularly outside the USA). Only two international geomathematical/computing journals are published (Computers & Geosciences; Mathematical Geology), compared with dozens covering, say, petrology or mineralogy. It also remains common practice for years (and $1000s) to be spent setting up computerized machines to produce large volumes of data in machine-readable form, and then for geologists to plot these by hand on a sheet of graph paper! Despite this, the use of numerical methods in geology has now begun to increase at a rate which implies a revolution of no less importance than the plate tectonic revolution of the 1960's -- one whose impact is beginning to be felt throughout the academic, commercial, governmental and private consultative geological communities (Merriam 1969, 1981c). Although a few pioneers have been publishing benchmark papers for some years, the routine usage of machine-based analytical techniques, and the advent of low-priced desk-top microcomputers, have successively enabled and now at last persuaded many more geologists to become both numerate and computerate. Merriam (1980) estimated that two decades of increasing awareness had seen the percentage of geomathematical papers (sensu lato) rise to some 15% of all geological literature; meanwhile, mineralogy-petrology and geochemistry had both fallen to a mere 5% each! In these Notes, geomathematics and numerical geology are used interchangeably, to cover applications of mathematics, statistics and computing to processing real geological data. However, as applications which primarily store or retrieve numbers (e.g. databases) are included, as well as those involving actual mathematical calculations, 'Numerical Geology' is preferred in the title. 'Geomathematics' in this sense should not be confused with 'geostatistics', now usually restricted to a specialised branch of geomathematics dealing with ore body estimation (§20). Reasons for studying Numerical Geology can be summarised as follows: (1) Volumes of new and existing numerical data: The British Geological Survey, the world's oldest, recently celebrated its 150th anniversary by establishing a National Geoscience data-centre, in which it is hoped to store all accumulated records on a computer (Lumsden & Flowarth 1986). Information already existing in the Survey's archives is believed to amount to tens or hundreds of Gb (i.e. = 1010-11 characters) and to be increasing by a few percent annually. The volumes of valuable data existing in the worM's geological archives, over perhaps 250 years of geological endeavour, must therefore be almost immeasurably greater. It is now routine even for students to produce hundreds or thousands of multi-element analyses for a single thesis, while national programs of geochemical sampling easily produce a million individual dement values. Such volumes of data simply cannot be processed realistically by manual means; they require mathematical and statistical manipulation on computers -- in some cases large computers. (2) Better use of coded/digitised data: In addition to intrinsically numerical (e.g. chemical) data, geology produces much information which can be more effectively used if numerically coded. For example, relatively little can be done with records of, say, 'limestone' and 'sandstone' in a borehole log, but very much more can be done if these records are numerically coded as 'limestone = 1' and 'sandstone = 2'. Via encoding, enormous volumes of data are opened to computer processing which would otherwise have lain dormant. More importantly, geological maps - perhaps the most important tool of the entire science - can themselves be digitised (turned into large sets of numbers), opening up vast new possibilities for manipulation, revision, scale-change and other improvements. (3) Intelligent data use: It is absurd to acquire large volumes of data and then not to interpret them fully. Field geologists observing an outcrop commonly split into two (or more) groups, arguing perhaps over the presence or absence of a preferred orientation in kyanite crystals on a schist foliation surface. The possibility of actually measuring these orientations and analyzing them statistically (§17) is rarely aired-- at last in this author's experience! Petrologists are equally culpable when they rely on X-Y or, at maximum 'sophistication', X-Y-Z (triangular) variation diagrams, in representing the evolution of igneous rocks which have commonly been analyzed for up to 50 elements! Whereas some geological controversies (especially those based on interpretation of essentially subjective field observations) cannot be resolved numerically, many others can and should be. This is not to say (as Lord Kelvin did) that quantitative science is the only good science, but qualitative treatment of quantitative data is rarely anything but bad science. (4) Literature search and data retrieval: Most research projects must begin with reviews of the literature and, frequently, with exhaustive compilations of existing data. These are essential if informed views on the topic are to be reached, existing work is not merely to be duplicated, and optimum use is to be made of available funding, The ever-expanding geological literature, however, makes such reviews and compilations increasingly time-consuming and expensive via traditional manual means. Use of the increasing number of both bibliographical and analytical databases (§3) is therefore becoming a prequisite for well-informed, high-quality research. (5) Unification of interests: In these days of inexorably increasing specialisation in ever narrower topics, brought about by the need to keep abreast of the exploding literature, numerical geology forms a rare bridge between different branches not only of geology but of diverse other sciences. The techniques covered in this book are equally applicable (and in many cases have been in routine use for far longer) in biology, botany, geography, medicine, psychology, sociology, zoology, etc. Within geology itself, most topics covered here are as valuable to the stratigrapher as to the petrologist. 'Numerical geologists' are thus in the unique (and paradoxical) position of being both specialists and non-specialists; they may have their own interests, but their numerical and computing knowledge can often help all of their colleagues. (6) Employment prospects: There is a clear and increasing demand for computerate/numerate geologists in nearly all employment fields. In Australia, whose economy is dominated by geology-related activities (principally mining), a comprehensive national survey (AMIRA 1985) estimated that A$40M per annum could be saved by more effective use of computers in geology. Professional computer scientists are also of course in demand, but the inability of some of their number to communicate with 'laymen' is legendary! Consequently, many finns have perpetual need for those rare animals who combine knowledge of computing and mathematics with practical geological experience. Their unique bridging role also means that numerical geologists are less likely to be affected by the vaguaries of the employment market than are more specialised experts. Rationale and aims of this book This is a highly experimental book, constituting the interim text for new (1988) courses in 'Numerical Geology' at the University of Western Australia. It is published in the Springer Lecture Notes in Earth Sciences series precisely because, as the rubric for this series has it, "the timeIiness of a manuscript is more important than its form, which may be unfinished or tentative." Readers are more than welcome to send constructive comments to the author, such that a more seasoned, comprehensive version can be created in due course. Readers' indulgence is meanwhile craved for the number of mistakes which must inevitably remain in a work involving so many citations and cross-references. Emphasis is particularly placed on the word Notes in the series rifle: this book is not a statistical or mathematical treatise. It is not intended to stand on its own, but rather to complement and target the existing literature. It is most emphatically not a substitute for sound statistical knowledge, and indeed, descriptions of each technique are deliberately minimized such that readers shouM never be tempted to rely on this book alone, but should rather read around the subject in the wealth of more authoritative statistical and geomathematical texts cited. In other words, this is a synoptic work, principally about 'how to do', 'when not to do', 'what are the alternatives' and 'where to find out more'. It aims specifically: (1) to introduce geologists to the widest possible range of numerical methods which have already appeared in the literature; and thus (2) to infuse geologists with just sufficient background knowledge that they can: (a) locate more detailed sources of information; (b) understand the broad principles behind interpreting most common geological problems quantitatively; (c) appreciate how to take best advantage of computers; and thereby (d) cope with the "information overload" (Griffiths 1974) which they increasingly face. Even these aims require the reader to become to some extent geologist, computer scientist, mathematician and statistician rolled into one, and a practical balance has therefore been attempted, in which just enough information is hopefully given to expedite correct interpretation and avoidance of pitfalls, but not too much to confuse or deter the reader. Despite the vast literature in mathematics, statistics and computing, and that growing in geomathematics, no previous book was found to fulfill these alms on its own. The range of methods covered here is deliberately much wider than in previous geomathematical textbooks, to provide at least an introduction to most methods geologists may encounter, but other books are consequently relied on for the detail which space here precludes. These Notes adopt a practical approach similar to that in language guidebooks -- at the risk of emulating the 'recipe book' abhorred in some quarters. Every Topic provides a minimum of highly condensed sketch-notes (fuller descriptions are included only where topics are not well covered in existing textbooks), complemented by worked examples using real data from as many fields of geology as space permits. Specialists should thereby be able to locate at least one example close to their problems of the moment. In the earlier (easier) topics, simple worked examples are calculated in full, and equations are given wherever practicable (despite their sometimes forbidding appearance), to enable readers not only to familiarise themselves with the calculations but also to experiment with their own data. In the later (multivariate) topics (where few but the sado-masochistic would wish to try the calculations by hand!), the worked examples comprise simplified output from actual software, to familiarise readers with the types of computer output they may have to interpret in practice. Topics were arranged in previous geomathematical textbooks by statistical subject: 'analysis of variance', 'correlation', 'regression', etc., while nonparametric (rank) methods were usually dealt with separately from classical methods (if at all). Here, topics are arranged by operation (what is to be done), and both classical and rank techniques are covered together, with similar emphasis. When readers know what they want to do, therefore, they need only look in one Topic for all appropriate techniques. The main difficulty of this work is the near impossibility of its goal-- though other books with similarly ambitious goals have been well enough received (e.g.J.Math.Geol. 18(5), 511-512). Some constraints have necessarily been imposed to keep the Notes of manageable size. Geophysics, for example, is sketchily covered, because (i) numerical methods are already far more integrated into most geophysics courses than geology courses; (ii) several recent textbooks (e.g. Cantina & Janecek 1984) cover the corresponding ground for geophysicists. Structural geology is less comprehensively covered or cited than, say, stratigraphy, because (a) it commands many applications of statistics and computing unto itself alone (e.g. 3-D modelling, 'unravelling' of folds), whereas these Notes aim at techniques equally applicable to most branches of geology; (b) excellent comprehensive reviews of structural applications are already available (e.g. Whitten 1969,1981). Remote sensing is also barely covered, since comprehensive source guides similar in purpose to the present one already exist (Carter 1986). For the sake of brevity, phrases throughout this book which refer to males are, with apologies to any whose sensitivities are thereby offended, taken to include females!

Description / Table of Contents: INTRODUCTION In the context of evolutionary studies, it is the privilege of paleontologists to trace the actual course of evolutionary change over time spans that are adequate for such a slow process. At the same time it is their crux that they can not always hope to do this with the resolution necessary to reveal the causal relationships involved. The Tübingen Sonderforschungsbereich 53, "Palökologie", was primarily geared to study the interrelationships between organisms and environments in the fossil record. As is pointed out in this volume, such an approach will necessarily emphasize the static aspect of this relationship, all the more since this is what we need for the practical purposes of facies recognition. This was clone during a time interval of thirteen years at the level of individual species and taxonomic groups ("Konstruktions-Morphologie"), of characteristic facies complexes ("Fossil-Lagerstätten") and of assemblages ("Fossil- VergeseIlschaftungen") with the aim to recognize general patterns that persist in spite of the historical and evolutionary changes in the biosphere. But as our project came closer to its end, the possible causal relationships between physical and evolutionary changes became more tangible. This trend is expressed by symposia devoted to the biological effects of long term tectonic changes (KULLMANN & SCHÖNENBERG, eds., 1983) and of short term physical events (EINSELE & SEILACHER, eds., 1982). But in retrospect it appears that the time scales of the environmental changes chosen were either too large or too small to reveal the mechanisms of evolutionary response. The present volume is the outcome of a symposium of the projects B 20 ("Bankungsrhythmen in sedimentologischer, ökologischer und diagenetischer Sicht", directed by U. BAYER), D 40 ("Analoge Gehäuse-Aberrationen bei Ammonoideen", directed by J. WIEDMANN) and D 60 ("Substratwechsel im marinen Benthos", directed by A. SEILACHER) in September, 1983. tt addresses environmental changes at time scales large enough to produce more than a local ecological response and short enough to observe evolutionary and/or migratory changes at the species and genus levels. It also focusses on basins which by various degrees of isolation provided suitable sites for "evolutionary experiments", such as lakes and marginal epicontinental basins. In a way, this book is a successor of the previous one on "Cyclic and event stratification" (EINSELE & SEILACHER, eds., 1982). Small scale cycles and events are the 'primitives' of a sedimentary sequence, the lowermost scale from which it can be deciphered. However, medium and long term physical cycles commonly impress sedimentological and lithological trends on the stratigraphic column which are accompanied by faunal replacements and cycles. But since sedimentation is controlled both by physical and biological processes, which are intercorrelated in complicated ways, we also need to decode the stratigraphic text. In this effort, paleontological and sedimentological interpretation must go hand in hand. On the 'megascale' of global sea-level changes faunal and species evolution is triggered by opening and closing of migration pathways, sometimes providing us with malor biostratigraphic boundaries. As it turns out, however, integrated research and the choice of suitable scales do not free us from problems of resolution. Thus our inability to distinguish local speciation from ecophenotypic modification and from immigration in the fossil record excludes definite evolutionary answers even in well studied cases. Nevertheless we hope that this approach opens a fruitful discussion, in which stratigraphy, systematic paleontology and paleoecology will be reconciled in a concerted effort to eventually understand the evolutionary mechanisms of our biosphere.

Description / Table of Contents: PREFACE It was only during the last few years, that the geological effects of storms and hurricanes in shallow-marine environments have been better appreciated. Not only were storm deposits recognized to dominate many shelf sequences, they also proved to be valuable tools in facies and paleogeographical analysis. Additionally, storm layers form important hydrocarbon reservoirs. Storm-generated sequences are now reasonably mell documented in terms of their facies associations in the stratigraphic record. Much less is known, however, about the effects and the depositional processes of modern storms, and about the styles of storm sedimentation on basinwide scales. Accordingly, the goal of this study is two-fold: 1. it presents two case studies of modern carbonate and terrigenous clastics storm sedimentatioq. The models derived from these actualistic examples can be used to interprete possible ancient analogues. 2. it presents a comprehensive analysis of an ancient storm depositional system (Muschelkalk) on a basin-wide scale. The underlying approach of this study is a process-oriented analysis of sedimentary sequences, an approach that ~as summarized by Matthews (1974, 1984) as "dynamic stratigraphy". The integration of actualistic models with a "dynamic" stratigraphic analysis helps to understand the dynamics of storm depositional systems; these models have a potential to be applied to other basins and to predict the facies organisation and the facies evolution in such systems...

Description / Table of Contents: The aim of this volume is to reflect the current state of geoscientific activity focused on the geodynamic evolution of the Atlas system and to discuss new results and ideas. The volume provides a selection of papers on the geological history, structural development, and geophysical data of Morocco. It was not possible to cover all areas of geoscientific interest, however, we hope to shed some light on the major geodynamic problems.

Description / Table of Contents: PREFACE Our planet is evolving and changing; its surface is capable of unleashing great violence as its crust is created and destroyed. Quite remarkably, it has been only recently that the fundamental elements of this evolution were fully appreciated, and only within the last decade have there been technologies capable of directly meastLring the global motions of the Earth's crust which are one of the most visible manifestations of these processes. Before the advent of space technologies, the nature of contemporary global plate motions went largely unobserved. These motions were understood from the geological records, and plate rates for million year averages were established_ Fortunately, the revolution in geophysics brought about by the general acceptance of plate tectonic theory has been paralleled by significant advances in space geodesy oceanography and geophysics. New space technologies have rapidly matured, yielding new insights and capabilities for more completely understanding the dynamical properties of the Earth, its oceans and atmosphere. Likewise, the evolving earth sciences capabilities from space are fostering new questions and goals made possible through the creative exploitation of satellite missions. A workshop entitled "The Interdisciplinary Role of Space Geodesy" was held in Erice, Italy, on the island of Sicily on July 23-29, 1988, to discuss the directions and challenges of space geodeys for the decades to come. This international gathering was made possible by the E. Majorana Centre for Scientific Culture int he framework of tis International School of Geodesy. The workshop was sponsored by the Italian Ministry of education, the Italian Ministry of Scientific and Technological Research, the Sicilian Regional Government, the Italian National Institute of Geophysics, and the National Aeronautics and Space Administration of the United States. This volume is the result of the dedicated effort undertaken by an international group of scientists and administrators who have contemplated the challenge of the future of space-based earth science for the next decade. Recognizing the need for defining new milestones both in science and technology, they have developed a detailed report of what could be achieved and what challenges remain after twenty fertile years of space exploration...

Description / Table of Contents: PREFACE The suggestion to compile and publish this volume dealing with some geoscientific problems of the Central Andes came up during a conference on "Mobility of Active Continental Margins" held in Berlin, February 1986. At this international conference, organized by the Berlin Research Group "Mobility of Active Continental Margins", colleagues from Europe, Southern and Northern America reported on their current investigations in the Central Andes. The Central Andes claim a special position in the 7000 km long Andean mountain range. In Northern Chile, Southern Bolivia and Northwest Argentina the Central Andes show their largest width with more than 650 km and along a Geotraverse between the Pacific coast and the Chaco all typical Andean morphotectonic units are well developed. Here, the pre-Andean evolution is documented by outcropping of Paleozoic and pre-Cambrian rocks. The characteristic phenomena of the Andean cycle can be studied along the entire geotraverse. The migration of the tectonic and magmatic activity starting in Jurassic and being active t i l l Quaternary is clearly evidenced. Besides the Himalaya, the Central Andes show with 70-80 km and -400 mgal the largest crustal thickness known in mountain ranges. These and many other interesting and exciting geoscientific features encouraged a group of geoscientists from both West-Berlin universities (Freie UniversitAt and Technische UniversitAt) to focus their studies along a geotraverse through the Central Andes. The realization of these studies would not have been possible without the active assistance and close cooperation of our colleagues from the geoscientific institutions in Salta (Argentina), La Paz and Santa Cruz (Bolivia) and Antofagasta and Santiago (Chile). Concerning the German participation, this joint and interdisciplinary project is financially supported since 1982 as Reserach Group" Mobility of Active Continental Margins" by the German Research Society and by the West-Berlin universities as well. A number of colleagues from universities in West Germany take part in this project, too. The papers presented here deal with the period from Late Precambrian up to the youngest phenomena in Quaternary. The contributions cover the whole spectrum of geoscientific research, geology, paleontology, petrology, geochemistry, geophysics and geomorphology. In conclusion, the data published here may help to improve the picture of Andean structure and evolution. The detailed investigations carried out in the past years show, that the first simple plate tectonic models proposed in the beginning of the seventies have to improved and modified. Furthermore, the results can be seen as contribution to the international Lithospheric Project and as a useful data base for the construction of a Central Andean Transect...

Description / Table of Contents: PREFACE During the last few years, evaporites have increasingly been regarded as sediments and not only as chemical precipitates. Especially the intensive study of the Zechstein facies has resulted in a vast amount of observations and interpretations which are of general significance, offering important information to all sedimentologists interested in carbonates and evaporites. It seems therefore useful to introduce the sedimentological approach in a basin where various chemical concepts have been developed. This is the aim of the present volume, and this approach will be recognized by the reader in most of the chapters. The idea of publishing a collection of papers on the Zechstein facies and related rocks found an enthusiastic response, although later some contributors were, for various reasons, unable to meet the deadline. However, the papers submitted cover all major fields and will certainly stimulate further research...

Description / Table of Contents: PREFACE In a densily populated industrialized country, waste disposal must be compatible with the requirements of the environment. This is one of the indispensable requirements to guarantee an effective protection of the environment. In the past years the waste disposal industry has been given increasing attention by the general public as well as the authorities. This confirms the necessity of adapting the quality of waste disposal to the technological standard of the production. While in the past, waste disposal performance was more or less evaluated in terms of short-term costs, there is at present a reorientation in the direction of a science-based waste disposal industry. These new tendencies are taking into account ecological factors as well as the long-term consequences - i.e., for decades and centuries to come - of waste disposal methods. In this light, particular attention is given to the depositing of residues whose utilization does not appear meaningful from an ecological point of view, or would require disproportionate ressources. It is an important concern of the Federal Authorities to encourage the rapid materialization of disposal solutions which can function as ultimate deposits, and which will therefore cause neither water pollution nor gaseous emissions. In view of this goal it is necessary to establish criteria and regulations for the wastes to be deposited as well as for the characteristics of the deposits. This field confronts science with an urgent but rewarding challenge and calls for close collaboration between many different specialized disciplines...

Description / Table of Contents: This book is the collection of the Lecture Notes of an International Summer School of Theoretical Geodesy held in Assisi (Italy) from May 23 to June 3 -1988.

Description / Table of Contents: Ein Integrationshandbuch im besten Sinne: Das Wissen um das Zusammenspiel von Microsoft Windows Server 2003, ADS, Windows XP Professional, Office XP/2003 oder Exchange Server ist sehr komplex. Administratoren, die nach einer Gesamtlösung suchen, stellen fest, dass es immens viele Informationen, Fehlerbeschreibungen, Service Packs, Patches und Hotfixes zu den Einzelprodukten gibt, aber keinen Lösungsansatz, der dieses Wissen bündelt und in Beziehung setzt. Anders dieses Buch: Schritt für Schritt wird ein Gesamtsystem implementiert, das nicht nur über einen kurzen Zeitraum läuft, sondern wartbar bleibt und später auf neue Versionen upgedated werden kann. Die 3. Auflage des Standardwerkes wurde aktualisiert und erweitert um Ausführungen zu Small Business Server, Windows Server 2003 R2, Windows Terminalserver, Access-based Enumeration und Best Practices zum Drucken im Netzwerk.

Description / Table of Contents: Wer Anwendungen mit Visual Basic 2008 programmieren will, findet in diesem Buch alles, was er dafür braucht. Neben dem Framework und der Entwicklungsumgebung Visual Studio sowie der Sprachsyntax von Visual Basic wird ausführlich auf die objektorientierte Programmierung eingegangen. Häufig verwendete Programmiertechniken werden ebenso gezeigt wie die Entwicklung grafischer Oberflächen mit WinForms und WPF sowie die Datenbankanbindung mit ADO.Net. Das Buch enthält alle Neuerungen des Visual Studio 2008. So werden die Themen LINQ (Language Integrated Query, ganz neu in .NET 3.5) oder etwa XAML (eXtensible Application Markup Language) sehr ausführlich in eigenen neuen Kapiteln behandelt.

Description / Table of Contents: Joomla! ist ein populäres Open-Source-CMS, das durch seine leichte Zugänglichkeit, Leistungsfähigkeit und Flexibilität besticht. Es basiert auf PHP und MySQL und kann daher auf verschiedensten Serverumgebungen eingesetzt werden. Der Versionssprung von 1.0 auf 1.5 macht es deutlich: umfangreiche Änderungen, wie z. B. die grundlegende Überarbeitung des Joomla!-Frameworks, Datenbankabstraktion und verbesserte Caching-Verfahren machen Joomla! 1.5 noch funktionsreicher, performanter und sicherer. Das Buch bietet eine umfassende Einführung in Installation, Funktionsumfang und Betrieb von Joomla! 1.5. Darüber hinaus werden auch professionelle Themen wie Websitemigration, Entwicklung von Erweiterungen und Datensicherung detailliert dargestellt.

Description / Table of Contents: Sie kennen sich mit Photoshop gut aus, suchen aber noch Tipps und Tricks für einen produktiveren Einsatz? Dieses Buch bietet reines Profiwissen! Im Fokus stehen hier Techniken für Fortgeschrittene, Hilfestellungen für einen effektiven Workflow und Tipps zur Automatisierung und Optimierung. So finden Sie Profiwissen z.B. zu den Themen Auswahlen, Effekte, Dritthersteller-Tools, Druckausgabe, Farbmanagement, Workflow, Bridge, Skripte, CameraRAW, Probleme mit Digitalfotos und vieles mehr. Grundlagenwissen wird hier nicht mehr erläutert! Ein Buch, das zum Schmökern einlädt und viele erhellende Zusammenhänge aufzeigt, Ihnen aber besonders hilft, Zeit zu sparen!

Description / Table of Contents: IOP Publishing presents Volume 6 of the open-access IOP Conference Series: Earth and Environmental Science (EES) as the online abstract book for the IARU International Scientific Congress on Climate Change: Global Risks, Challenges and Decisions (10–12 March, Copenhagen, Denmark). This abstracts-only volume of EES is quite different to standard IOP Conference Series proceedings volumes which contain full, peer-reviewed proceedings papers. This unique volume of more than 1400 abstracts, divided into 58 different sessions, contains all the oral and poster presentations from the Congress. In view of the importance of the Climate Change Congress as a scientific basis for the COP15 conference, we are delighted to offer this collection as a permanent record of current research devoted to climate change. We hope this compilation will contribute to future world-wide dialogue on climate change in the ongoing search to address the scientific, political, social and economic challenges ahead.

Description / Table of Contents: Linux-Nutzer, die bei Einrichtung und Verwaltung ihres Systems großen Wert auf Unabhängigkeit legen, greifen zu Gentoo Linux. Herz einer jeden Gentoo-Installation ist Portage, ein fortschrittliches, den FreeBSD-Ports ähnliches Paketmanagementsystem. Anders als die Paketmanager anderer Distributionen setzt Portage nicht auf vorkompilierte Binärpakete, sondern arbeitet auf Quellcodebasis. Portage sowie die Vor- und Nachteile quellbasierten Paketmanagements allgemein bilden Kernthemen dieses Buches. Der Autor führt praxisnah durch Installation und Administration und beschreibt Besonderheiten insbesondere für jene, die bereits Erfahrung mit anderen Linux-Distributionen gesammelt haben, so dass auch versierte Anwender Neues über die Konzepte von Linux bzw. das Zusammenspiel seiner Komponenten erfahren. Als Beispielszenario dient das Einrichten eines Webservers. Das Buch zeigt darüber hinaus, wie man die Distribution selbst erweitert und den eigenen Rechner in ein maßgeschneidertes Linux-System verwandelt gemäß dem Motto des Projekts: "Gentoo is all about choices".

Description / Table of Contents: Niemals zuvor lag die Macht zur Kontrolle von Kreativität derart konzentriert in der Hand einiger weniger – der Medienindustrie. Gemäß ihren wirtschaftlichen Interessen erstickt sie schöpferische Prozesse oder zwingt diese in für sie einträgliche Bahnen. Unsere Gesellschaft steht für den freien Markt ebenso wie für die Freiheit der Rede; warum aber lässt sie eine solche Bevormundung zu? Indem wir mit unserer Tradition der freien Kultur brechen, so zeigt Lawrence Lessig, "der bedeutendste Denker zum Thema geistiges Eigentum im Internet-Zeitalter" ("The New Yorker"), verlieren wir die Freiheit zur Kreativität und zuletzt auch die Freiheit, Neues zu denken. Mit Hartmut Pilch, dem Vorsitzenden des FFII, und Annegret Claushues haben wir zwei fachlich wie sprachlich hochkompetente Übersetzer gewinnen können, die Inhalt und Form des Textes jederzeit gerecht werden.

Description / Table of Contents: The Beyond Kyoto conference in Aarhus March 2009 was organised in collaboration with other knowledge institutions, businesses and authorities. It brought together leading scientists, policy-makers, authorities, intergovernmental organisations, NGO's, business stakeholders and business organisations. The conference was a joint interdisciplinary project involving many academic areas and disciplines. These conference proceedings are organised in central and recurring themes that cut across many debates on climate change, the climatic challenges as well as the solutions. In the front there is a short presentation of the conference concept. Part I of the proceedings focuses on issues related to the society – covering climate policy, law, market based instruments, financial structure, behaviour and consumption, public participation, media communication and response from indigenous peoples etc. Part II of the proceedings concerns the scientific knowledge base on climate related issues – covering climate change processes per se, the potential impacts of projected climate change on biodiversity and adaptation possibilities, the interplay between climate, agriculture and biodiversity, emissions, agricultural systems, increasing pressure on the functioning of agriculture and natural areas, vulnerability to extreme weather events and risks in respect to sea-level rise etc...

Description / Table of Contents: The Hiroshi Wakita Volume I is a collection of original papers regarding the role of terrestrial fluids in earthquake and volcanic processes. The importance of monitoring volcanic gases for studying volcanic eruptions is widely recognized by the scientific community. On the other hand, the usefulness of hydrologic and geochemical monitoring in earthquake studies, especially in earthquake prediction, has been controversial. This Pure and Applied Geophysics volume provides the results of some of the most recent studies on terrestrial fluids involved in both processes. The volume honors Hiroshi Wakita for his scientific contributions. Volume II will be published later in 2006. Both volumes should be useful to researchers and graduate students in the field.

Description / Table of Contents: Tsunamis like the Indian Ocean tsunami caused by the Sumatra-Andaman earthquake in 2004 or the Chilean earthquake in the Pacific Ocean in 1960 motivate international collaborations for the development of tsunami warning systems. Since 1960 the Tsunami Commission, established by the International Union of Geodesy and Geophysics, has been holding a biannual International Tsunami Symposium (ITS). This volume contains 20 contributions of leading scientists mostly presented at the 22nd International Tsunami Symposium held in summer 2005 in Greece. Consolidated findings based on hydrophone records, seismometer readings, and tide gauges are presented. Reports of post-tsunami surveys and numerical simulations for tsunamis such as the 2004 Indian Ocean event, as well as geological studies of tsunamis in Japan, Central and North America are given. Probabilistic tsunami hazard analysis and tsunami warning systems, among others, are described as are methods to predict tsunamis and mitigate their hazards.

Description / Table of Contents: This topical volume of the Journal of Pure and Applied Geophysics utilizes new information not previously accessible for fog related research. It focuses on surface and remote sensing observations of fog, various numerical model applications using new parameterizations, fog climatology, and new statistical methods. The results presented in this special issue come from research efforts in North America and Europe, mainly from the Canadian Fog Remote Sensing And Modeling (FRAM) and European COST-722 fog/visibility related projects. Students, postgraduates, and researchers, interested in cloud physics, physical meteorology, aviation meteorology, climate, weather forecasting, and in other adjacent disciplines, can use this book as a basis for future developments in fog research. It is hoped that this book will lead to new scientific challenges in fog related research, teaching, and applications.

Description / Table of Contents: Exciting developments in earthquake science have benefited from new observations, improved computational technologies, and improved modeling capabilities. Designing realistic supercomputer simulation models for the complete earthquake generation process is a grand scientific challenge due to the complexity of phenomena and range of scales involved from microscopic to global. The book is divided into two parts: The present volume - Part I - focuses on microscopic simulation, scaling physics, dynamic rapture and wave propagation, earthquake generation, cycle and seismic pattern. Topics covered range from numerical developments, rupture and gouge studies of the particle model, Liquefied Cracks and Rayleigh Wave Physics, studies of catastrophic failure and critical sensitivity, numerical and theoretical studies of crack propagation, developments in finite difference methods for modeling faults, long time scale simulation of interacting fault systems, modeling of crustal deformation, through to mantle convection.

Description / Table of Contents: Weather and climate are of concern to virtually all countries worldwide. For many countries the economy depends largely on agriculture, which is significantly affected by variations in weather and climate. This volume contains many original findings on weather and climate related to atmospheric and oceanic processes through mathematical modeling, numerical simulations, and field experiments and it will be useful as a reading material in graduate level courses dealing with weather, climate, boundary layer and air quality. The scientific community at large, especially younger scientists, will find this book a useful addition to their personal and institutional libraries.

Description / Table of Contents: The Palaeoproterozoic era (2500–1600 Ma) was a critical period of Earth history, with dynamic evolution from the deep planetary interior to its surface environment. Several lines of geological evidence suggest the existence of at least one pre-Rodinia supercontinent, named Nuna or Columbia, which formed near the end of Palaeoproterozoic time. Prior to this assembly, there may have been an older supercontinent (Kenorland) or perhaps only independently drifting supercratons. The tectonic records of amalgamation and dispersal of these ancient landmasses provide a framework that links processes of the deep Earth with those of its fluid envelope. The sixteen papers in this volume present reviews and new analytical data that span the geological record of Palaeoproterozoic Earth and provide a current picture of Palaeoproterozoic research. The volume provides a useful reference book for students and professional geoscientists interested in this important period of global evolution.

Description / Table of Contents: The Devonian was a critical period with respect to the diversification of early terrestrial ecosystems. The geotectonic setting was characterized by the switch from the post-Caledonian to the pre-Variscan situation. Plant life on land evolved from tiny tracheophytes to trees of considerable size in combination with a global increase in terrestrial biomass, and vertebrates started to conquer the land. Extensive shallow-marine areas and continental lowlands with a wide range of different habitats existed. These are preserved in a large number of basins all around the world. Climate change finally led from greenhouse to icehouse conditions towards the end of the Devonian. Rapid evolution of terrestrial ecosystems and climate change had a pronounced influence on sedimentation and biodiversity, not only in the terrestrial, but also in the marine realm. This volume contains case studies from Australia, China, Europe, South America and North America, and individual palaeoecosystems and their components have been investigated in different palaeogeographic settings that contribute to a much better understanding of the Devonian Period. This is a contribution to the IGCP 499 project on "Devonian land-sea interaction: evolution of ecosystems and climate".

Description / Table of Contents: Thermochronology - the use of temperature-sensitive radiometric dating methods to reconstruct the thermal histories of rocks - has proved to be an important means of constraining a wide variety of geological processes. Fission track and (U–Th)/He analyses of apatites, zircons and titanites are the best-established and most sensitive methods for reconstructing such histories in the uppermost kilometres of the crust, over time scales of millions to hundreds of millions of years. The papers published in this volume are divided into two sections. The first section on ‘New approaches in thermochronology’, presents the most recent advances of existing thermochronological methods and demonstrates the progress in the development of alternative thermochronometers and modelling techniques. The second section, ‘Applied thermochronology’, comprises original papers about denudation, long-term landscape evolution and detrital sources from the European Alps, northwestern Spain, the Ardennes, the Bohemian Massif, Fennoscandia and Corsica. It also includes case studies from the Siberian Altai, Mozambique, South Africa and Dronning Maud Land (East Antarctica) and reports an ancient thermal anomaly within a regional fault in Japan.

Description / Table of Contents: The detachment era (1977–1982) and its role in revolutionizing continental tectonics / B. Wernicke / Geological Society, London, Special Publications, 321, 1-8, 14 October 2009, https://doi.org/10.1144/SP321.1 --- The frictional strength of granular fault gouge: application of theory to the mechanics of low-angle normal faults / Carolyn Boulton, Tim Davies and Mauri McSaveney / Geological Society, London, Special Publications, 321, 9-31, 14 October 2009, https://doi.org/10.1144/SP321.2 --- Upper and lower crustal evolution during lithospheric extension: numerical modelling and natural footprints from the European Alps / Anna Maria Marotta, Maria Iole Spalla and Guido Gosso / Geological Society, London, Special Publications, 321, 33-72, 14 October 2009, https://doi.org/10.1144/SP321.3 --- Reconciling short- and long-term measures of extension in continental back arcs: heat flux, crustal structure and rotations within central North Island, New Zealand / T. A. Stern / Geological Society, London, Special Publications, 321, 73-87, 14 October 2009, https://doi.org/10.1144/SP321.4 --- Cretaceous felsic volcanism in New Zealand and Lord Howe Rise (Zealandia) as a precursor to final Gondwana break-up / A. J. Tulloch, J. Ramezani, N. Mortimer, J. Mortensen, P. van den Bogaard and R. Maas / Geological Society, London, Special Publications, 321, 89-118, 14 October 2009, https://doi.org/10.1144/SP321.5 --- Structure and evolution of the western Corinth Rift, through new field data from the Northern Peloponnesus / Emmanuel Skourtsos and Haralambos Kranis / Geological Society, London, Special Publications, 321, 119-138, 14 October 2009, https://doi.org/10.1144/SP321.6 --- Timing and nature of formation of the Ios metamorphic core complex, southern Cyclades, Greece / Stuart N. Thomson, Uwe Ring, Stephanie Brichau, Johannes Glodny and Thomas M. Will / Geological Society, London, Special Publications, 321, 139-167, 14 October 2009, https://doi.org/10.1144/SP321.7 --- Timing of the Amorgos detachment system and implications for detachment faulting in the southern Aegean Sea, Greece / Uwe Ring, Stuart N. Thomson and Gideon Rosenbaum / Geological Society, London, Special Publications, 321, 169-178, 14 October 2009, https://doi.org/10.1144/SP321.8 --- Cenozoic tectonic evolution of Naxos Island through a multi-faceted approach of fission-track analysis / Diane Seward, Olivier Vanderhaeghe, Luc Siebenaller, Stuart Thomson, Christian Hibsch, Anatol Zingg, Patrick Holzner, Uwe Ring and Stephanie Duchêne / Geological Society, London, Special Publications, 321, 179-196, 14 October 2009, https://doi.org/10.1144/SP321.9 --- Syn-extensional granitoids in the Menderes core complex and the late Cenozoic extensional tectonics of the Aegean province / Yildirim Dilek, Şafak Altunkaynak and Zeynep Öner / Geological Society, London, Special Publications, 321, 197-223, 14 October 2009, https://doi.org/10.1144/SP321.10 --- A case study of lateral spreading: the Precambrian Svecofennian Orogen / Annakaisa Korja, Paula Kosunen and Pekka Heikkinen / Geological Society, London, Special Publications, 321, 225-251, 14 October 2009, https://doi.org/10.1144/SP321.11

Description / Table of Contents: Accretionary orogens form at convergent plate boundaries and include the supra-subduction zone forearc, magmatic arc and backarc components. They can be broken into retreating and advancing types, based on their kinematic framework and resulting geological character. Accretionary systems have been active throughout Earth history, extending back until at least 3.2 Ga, and provide an important constraint on the initiation of horizontal motion of lithospheric plates on Earth. Accretionary orogens have been responsible for major growth of the continental lithosphere, through the addition of juvenile magmatic products, but are also major sites of consumption and reworking of continental crust through time. The aim of this volume is to provide a better understanding of accretionary processes and their role in the formation and evolution of the continental crust. Fourteen papers deal with general aspects of accretion and metamorphism and discuss examples of accretionary orogens and crustal growth through Earth history, from the Archaean to the Cenozoic.

Description / Table of Contents: Founded in 1807, the Geological Society of London became the world's first learned society devoted to the Earth sciences. In celebration of the Society's 200-year history, this book commemorates the lives of the Society's 13 founders and sets geology in its national and European context at the turn of the nineteenth century. In Britain, geology was emerging as a subject in its own right from three closely related disciplines - chemistry, mineralogy and medicine - disciplines that reflect the principal professions and interests of the founders. The tremendous energy and cooperation of these 13 men, about whom little was previously known, quickly mobilized like-minded men around the country and fuelled the nation's passion for geology; an enthusiasm that soon spread to America and Australia. Two previously unpublished works from this period, essential to understanding the founding of the Society, are reproduced here for the first time. The book closes with a review of the Society's 2007 Bicentenary celebrations.

Description / Table of Contents: Magmas are subject to a series of processes that lead to their differentiation during transfer through, and storage within, the Earth's crust. The depths and mechanisms of differentiation, the crustal contribution to magma generation through wall-rock assimilation, the rates and timescales of magma generation, transfer and storage, and how these link to the thermal state of the crust are subject to vivid debate and controversy. This volume presents a collection of research articles that provide a balanced overview of the diverse approaches available to elucidate these topics, and includes both theoretical models and case studies. By integrating petrological, geochemical and geophysical approaches, it offers new insights to the subject of magmatic processes operating within the Earth's crust, and reveals important links between subsurface processes and volcanism.

Description / Table of Contents: This book deals with various interesting aspects of the histories of geomorphology and Quaternary geology in different parts of the world. The papers cover a range of topics: the origin of the term ‘Quaternary’, histories of ideas and debates relating to aspects of fluvial geomorphology (USA and Australia), glacial geomorphology and glaciation (Northern Europe, the Baltic countries, Russia, Iceland, and New Zealand), desert dunes and the geology of Australia, peneplains in China, a palaeo-Tokyo Bay in Japan, together with biographies of Charles Cotton (New Zealand), Valerija Cepulyte (Lithuania) and Ceslovas Pakuckas (Lithuania and Poland) that highlight their respective contributions to the disciplines of geomorphology and Quaternary geology. There is an autobiographical contribution from E. E. Milanovsky (Russia) on his work in Siberia, the Caucasus and Iceland, illustrated by his sketches made in the field.

Description / Table of Contents: This book is the first to describe the history of geoconservation. It draws on experience from the UK, Europe and further afield, to explore topics including: what is geoconservation; where, when and how did it start; who was responsible; and how has it differed across the world? Geological and geomorphological features, processes, sites and specimens, provide a resource of immense scientific and educational importance. They also form the foundation for the varied and spectacular landscapes that help define national and local identity as well as many of the great tourism destinations. Mankind's activities, including contributing to enhanced climate change, pose many threats to this resource: the importance of safeguarding and managing it for future generations is now widely accepted as part of sustainable development. Geoconservation is an established and growing activity across the world, with more participants and a greater profile than ever before. This volume highlights a history of challenges, set-backs, successes and visionary individuals and provides a sound basis for taking geoconservation into the future.

Description / Table of Contents: Twenty years have passed since Menzies & Hawkesworth extended the concept of metasomatism to mantle processes. The aim of this book is to gather together progress made on this topic since then. Most of the 14 papers reported in the volume rely on in situ major and trace element analyses of minerals and glasses in mantle xenoliths, and deal with different kinds of metasomatic agents at variable fluid/rock ratios in tectonic settings as different as intra-plate, mid-ocean ridge (ophiolites) and supra-subduction. The book contributes to the wide debate on the nature of the fluids migrating into the mantle wedge, as well as on the different residential times of the subduction signature. In addition papers on intra-plate settings deal with the problem of relating various metasomatic signatures to one single metasomatic event through an infiltration-reaction process.

Description / Table of Contents: Restraining and releasing bends are common, but enigmatic features of strike-slip fault systems occurring in all crustal environments and at regional to microscopic scales of observation. Regional-scale restraining bends are sites of mountain building, transpressional deformation and basement exhumation, whereas releasing bends are sites of topographic subsidence, transtensional deformation, basin sedimentation and possible volcanism and economic mineralization. Because restraining and releasing bends often occur as singular self-contained domains of complex deformation, they are appealing natural laboratories for Earth scientists to study fault processes, earthquake seismology, active faulting and sedimentation, fault and fluid-flow relationships, links between tectonics and topography, tectonic and erosional controls on exhumation, and tectonic geomorphology. This volume addresses the tectonic complexity and diversity of strike-slip restraining and releasing bends with 18 contributions divided into four thematic sections: (1) a topical review of fault bends and their global distribution; (2) bends, sedimentary basins and earthquake hazards; (3) restraining bends, transpressional deformation and basement controls on development; (4) releasing bends, transtensional deformation and fluid flow.

Description / Table of Contents: The Proterozoic and early Phanerozoic was a time punctuated by a series of significant events in Earth history. Glaciations of global scale wracked the planet, interfingered with dramatic changes in oceanic and atmospheric chemistry and marked changes in continental configuration. It was during these dynamic and ‘weedy’ times that metazoans first appeared. Their subsequent diversification culminated in the appearance of hard tissue skeletons and deep "farming" of the marine substrate in late Proterozoic and first few millions of years of the Phanerozoic. The papers in this book deal specifically with the precise timing of physical events and teasing out of the effects which these changing environments, climates, global chemistry and palaeogeography had on the development and diversification of animals, resulting in the spectacular Ediacaran/Vendian faunas of the late Precambrian.

Description / Table of Contents: The book presents an overview of the main hazards affecting karst, including collapse and subsidence phenomena, hydrological hazards and human-induced geohazards. Consideration is also given to the problems of geohazard management in karst. The geological and hydrological properties of karst terrains make them among the most fragile in the world and pose serious problems for land managers. Sustainable development in these terrains requires efforts to limit geohazards of anthropogenic origin and to recognize and mitigate against those of natural origin. Aimed at providing the reader with worldwide case studies, the contributions cover a range of geological and morphological settings. Geographically, the fourteen papers discuss very different karst areas, from North America, the Caribbean and Asia to several karst areas in Europe, including the British Isles, Spain, France and Italy.

Description / Table of Contents: There has lately been a growth in the number and level of studies of contourite deposits. Most recent studies of contourites have two major lines of interest. One, propelled by the oil industry's continuous move into increasingly deep waters, concerns their economic significance. The other involves the stratigraphic/ palaeoceanographic record of ocean circulation changes imprinted on contourite deposits that can be a key to understanding better the climate-ocean connection. The application of many different theoretical, experimental and empirical resources provided by geophysics, sedimentology, geochemistry, petrology, scale modeling and field geology are used in the 16 papers of this volume, proposing answers to those two main aspects. The papers are subdivided into two major categories (economic interest and stratigraphic/palaeoceanographic significance), with case studies ranging from well-documented drifts to new examples of modern and fossil series, involving a large diversity of geographic and physiographic scenarios worldwide.

Description / Table of Contents: This Special Publication, in memory and celebration of the work of Professor Mike Coward, is about the deformation of the continental lithosphere. The collected papers discuss geometry, structural principles, processes and problems in a wide range of tectonic settings and thereby reflect the breadth of Coward's interests. They encompass the evolution of Precambrian basement gneiss terrains, the geometry and evolution of thrust systems, basement involvement and structural inheritance in basins, syn-orogenic extension, salt tectonics, the implication of structural evolution on hydrocarbon prospectivity and structural controls on mineralization. Examples are drawn from the Lewisian and Moine Thrust Belt of NW Scotland, the Italian Apennines, NW Himalayas, the Cyclades, Oman, Zagros Mountains, Colombian Cordillera, Carpathians, North Sea, offshore Brazil, regional studies of the Irumide Belt (central Africa), Taurus Mountains (Turkey), greater South America, and from the Witwatersrand Basin of South Africa and the Antler Orogeny of SW USA.

Description / Table of Contents: This collection of 27 review and research papers provides an overview of the geodynamic concepts of channel flow and ductile extrusion in continental collision zones. The focal point tor this volume is the proposal that the middle or lower crust acts as a ductile, partially molten channel flowing out from beneath areas of over-thickened crust, such as the Tibetan plateau, towards the topographic surface at plateau margins. This controversial proposal explains many features related to the geodynamic evolution of the plateau and, for example, extrusion and exhumation of the crystalline core of the Himalayan mountain chain to the south. In this volume thermal-mechanical models for channel flow, extrusion and exhumation are presented, and geological and geophysical evidence both for and against the applicability of such models to the Himalayan-Tibetan Plateau system, as well as older continental collision zones such as the Hellenides, the Appalachians and the Canadian Cordillera, are discussed.

Description / Table of Contents: Since Karl Pearson wrote his paper on spurious correlation in 1897, a lot has been said about the statistical analysis of compositional data, mainly by geologists such as Felix Chayes. The solution appeared in the 1980s, when John Aitchison proposed to use Iogratios. Since then, the approach has seen a great expansion, mainly building on the idea of the ‘natural geometry’ of the sample space. Statistics is expected to give sense to our perception of the natural scale of the data, and this is made possible for compositional data using Iogratios. This publication will be a milestone in this process. This book will be of interest to geologists using statistical methods. It includes the intuitive justification of the methodology, convincing through case studies and presenting user-friendly software, which includes a section for those who need to see the proof of the mathematical consistency of the methods used.

Description / Table of Contents: High-latitude settings are sensitive to climatically driven palaeoenvironmental change and the resultant biotic response. Climate change through the peak interval of Cretaceous warmth, Late Cretaceous cooling, onset and expansion of the Antarctic ice sheet, and subsequently the variability of Neogene glaciation, are all recorded within the sedimentary and volcanic successions exposed within the James Ross Basin, Antarctica. This site provides the longest onshore record of Cretaceous-Tertiary sedimentary and volcanic rocks in Antarctica and is a key reference section for Cretaceous-Tertiary global change. The sedimentary succession is richly fossiliferous, yielding diverse invertebrate, vertebrate and plant fossil assemblages, allowing the reconstruction of both terrestrial and marine systems. The papers within this volume provide an overview of recent advances in the understanding of palaeoenvironmental change spanning the mid-Cretaceous to the Neogene of the James Ross Basin and related biotic change, and will be of interest to many working on Cretaceous and Tertiary palaeoenvironmental change.

Description / Table of Contents: Twenty-four years have elapsed since the publication of Halbouty’s AAPG Memoir of 1982, The Deliberate Search for the Subtle Trap. Since then, the technologies employed in hydrocarbon exploration have become extraordinarily sophisticated, yet current exploration for stratigraphic traps is to some extent restricted to areas where seismic data simplifies exploration by allowing direct inference of fluid fill and reservoir development. This Special Publication draws upon contributions that examine current industry perceptions of stratigraphic trap exploration and the technologies, tools and philosophies employed in such exploration, given the changing industry environment. This book contains a collection of papers examining a number of themes related to exploration for stratigraphic traps, ranging from play and risk assessment, through regional assessments of stratigraphic trapping potential, specific exploration programmes targeted at stratigraphic traps to specific working traps and plays where stratigraphic trapping is prevalent.

Description / Table of Contents: Rock features are important traces of the formation and development of karst surface. On various karren their record is especially rich, revealing to us the many factors that in diverse conditions formed the karst surface on various carbonate and other rock. We have tried to present the most characteristic rock features and through them the most important factors and processes in the formation of the karst surface, the methods of studying them, and the most outstanding examples. Forty-nine contributing authors offer a wide spectrum of content and examples of rock forms from many karst regions around the world. During the preparation of the book, many new and interesting discoveries emerged that strongly encouraged further research into this extremely indicative and often esthetically attractive part of our karst natural heritage.

Description / Table of Contents: This book provides an overview of the principal environments, main processes and manifestations of hypogenic speleogenesis, and refines the relevant conceptual framework. It consolidates the notion of hypogenic karst as one of the two major types of karst systems (the other being epigenetic karst). Karst is viewed in the context of regional groundwater flow systems, which provide the systematic transport and distribution mechanisms needed to produce and maintain the disequilibrium conditions necessary for speleogenesis. Hypogenic and epigenic karst systems are regularly associated with different types, patterns and segments of flow systems, characterized by distinct hydrokinetic, chemical and thermal conditions. Epigenic karst systems are predominantly local systems, and/or parts of recharge segments of intermediate and regional systems. Hypogenic karst is associated with discharge regimes of regional or intermediate flow systems. Various styles of hypogenic caves that were previously considered unrelated, specific either to certain lithologies or chemical mechanisms are shown to share common hydrogeologic genetic backgrounds. In contrast to the currently predominant view of hypogenic speleogenesis as a specific geochemical phenomenon, the broad hydrogeological approach is adopted in the book. Hypogenic speleogenesis is defined with reference to the source of fluid recharge to the cave-forming zone, and type of flow system. It is shown that confined settings are the principal hydrogeologic environment for hypogenic speleogenesis. However, there is a general evolutionary trend for hypogenic karst systems to lose their confinement due to uplift and denudation and due to their own expansion. Confined hypogenic caves may experience substantial modification or be partially or largely overridden under subsequent unconfined (vadose) stages, either by epigenic processes or continuing unconfined hypogenic processes, especially when H2S dissolution mechanisms are involved. Hypogenic confined systems evolve to facilitate cross-formational hydraulic communication between common aquifers, or between laterally transmissive beds in heterogeneous soluble formations, across cave-forming zones. The latter originally represented low-permeable, separating units supporting vertical rather than lateral flow. Layered heterogeneity in permeability and breaches in connectivity between different fracture porosity structures across soluble formations are important controls over the spatial organization of evolving ascending hypogenic cave systems. Transverse hydraulic communication across lithological and porosity system boundaries, which commonly coincide with major contrasts in water chemistry, gas composition and temperature, is potent enough to drive various disequilibrium and reaction dissolution mechanisms. Hypogenic speleogenesis may operate in both carbonates and evaporites, but also in some clastic rocks with soluble cement. Its main characteristic is the lack of genetic relationship with groundwater recharge from the overlying or immediately adjacent surface. It may not be manifested at the surface at all, receiving some expression only during later stages of uplift and denudation. In many instances, hypogenic speleogenesis is largely climate-independent. There is a specific hydrogeologic mechanism inherent in hypogenic transverse speleogenesis (restricted input/output) that suppresses the positive flow-dissolution feedback and speleogenetic competition in an initial flowpath network. This accounts for the development of more pervasive channeling and maze patterns in confined settings where appropriate structural prerequisites exist. As forced-flow regimes in confined settings are commonly sluggish, buoyancy dissolution driven by either solute or thermal density differences is important in hypogenic speleogenesis. In identifying hypogenic caves, the primary criteria are morphological (patterns and meso-morphology) and hydrogeological (hydrostratigraphic position and recharge/flow pattern viewed from the perspective of the evolution of a regional groundwater flow system). Elementary patterns typical for hypogenic caves are network mazes, spongework mazes, irregular chambers and isolated passages or crude passage clusters. They often combine to form composite patterns and complex 3-D structures. Hypogenic caves are identified in various geological and tectonic settings, and in various lithologies. Despite these variations, resultant caves demonstrate a remarkable similarity in cave patterns and meso-morphology, which strongly suggests that the hydrogeologic settings were broadly identical in their formation. Presence of the characteristic morphologic suites of rising flow with buoyancy components is one of the most decisive criteria to identify hypogenic speleogenesis. Hypogenic speleogenesis is much more widespread than it was previously presumed. Hypogenic caves include many of the largest, by integrated length and by volume, documented caves in the world. The refined conceptual framework of hypogenic speleogenesis has broad implications in applied fields and promises to make karst and cave expertise more demanded by practicing hydrogeology, geological engineering, economic geology and mineral resource industries. Any generalization of hydrogeology of karst aquifers, as well as approaches to practical issues and resource prospecting in karst regions, should take into account the different nature and characteristics of hypogenic and epigenic karst systems. Hydraulic properties of karst aquifers, evolved in response to hypogenic speleogenesis, are characteristically different from epigenic karst aquifers. In hypogenic systems, cave porosity is roughly an order of magnitude greater, and areal coverage of caves is five times greater than in epigenic karst systems. Hypogenic speleogenesis commonly results in more isotropic conduit permeability pervasively distributed within highly karstified areas measuring up to several square kilometers. Although being vertically and laterally integrated throughout conduit clusters, hypogenic systems, however, do not transmit flow laterally for considerable distances. Hypogenic speleogenesis can affect regional subsurface fluid flow by greatly enhancing initially available cross-formational permeability structures, providing higher local vertical hydraulic connections between lateral stratiform pathways for groundwater flow, and creating discharge segments of flow systems, the areas of low-fluid potential recognizable at the regional scale. Discharge of artesian karst springs, which are modern outlets of hypogenic karst systems, is often very large and steady, being moderated by the high karstic storage developed in the karstified zones and by the hydraulic capacity of an entire artesian system. Hypogenic speleogenesis plays an important role in conditioning related processes such as hydrothermal mineralization, diagenesis, and hydrocarbon transport and entrapment. The appreciation of the wide occurrence of hypogenic karst systems, marked specifics in their origin, development and characteristics, and their scientific and practical importance, calls for revisiting and expanding of the current predominantly epigenic paradigm of karst and cave science.

Description / Table of Contents: The Early-Middle Pleistocene transition (around 1.2 to 0.5 Ma) marks a profound shift in Earth’s climate state. Low-amplitude 41 ka climate cycles, dominating the earlier part of the Pleistocene, gave way progressively to a 100 ka rhythm of increased amplitude that characterizes our present glacial—interglacial world. This volume assesses the biotic and physical response to this transition both on land and in the oceans: indeed it examines the very nature of Quaternary climate change. Milankovitch theory, palaeoceanography using isotopes and microfossils, marine organic geochemistry, tephrochronology, the record of loess and soil deposition, terrestrial vegetationa! change, and the migration and evolution of hominins as well as other large and small mammals, are all considered. These themes combine to explore the very origins of our present biota.

Description / Table of Contents: Sie setzen Adobe Photoshop CS4 oder Photoshop CS4 Extended professionell ein und müssen täglich unterschiedlichste Aufgabenstellungen lösen? Dann sind Sie sicher immer auf der Suche nach effizienten Problemlösungen, offen für neue Ideen und wollen auf dem neuesten Stand der (Photoshop-)Technik bleiben. Dieses Buch hilft Ihnen, über den Tellerrand zu schauen und vom fortgeschrittenen Anwender zum Photoshop-Profi zu werden. Lernen Sie, Probleme bei Digitalfotos zu beheben: Rauschen, Moiré, Unschärfe, Pixelfehler, Optische Verzerrungen. Trauen Sie sich, neue Wege zu gehen beim Einsatz altbekannter Funktionen wie Freistelltechniken, Masken, Kanälen und dem LAB-Modus -- oder setzen Sie gezielt alternative Programme von Drittanbietern ein. Dabei zeigt das Buch Strategien für die Anwendungsbereiche Fotobearbeitung, Videobearbeitung, Druckvorstufe, Web und 3D. Themen sind u.a. Camera Raw, HDR, Panoramen, Compositings & Montagen, Farb- und Tonwertkorrekturen, Farbmanagement, Sonderfarben, Filter, Animation, Workflow mit Dreamweaver, Fireworks und CS4-Videoprogrammen. Für die Beschleunigung Ihrer Arbeit gibt es außerdem Tipps zur Automatisierung, zum Scripten mit Photoshop und Flex, zum Teamwork und zur Versionierung. So schöpfen Sie das Potenzial von Photoshop CS4 wirklich aus!

Description / Table of Contents: This is volume I of the two-volume special issue Scattering and Attenuation of Seismic Waves which will contain total 17 invited review papers and about 30 c- tributed papers. The scope and contents of the special issue are described in the following Introduction. This volume includes 21 contributed papers arranged in the following order: Scattering theory and modeling including the scattering attenuation and its separation from the intrinsic attenuation; numerical method and simulation; field observation including coda Q and surface wave Q measurement; inversion; laboratory attenuation measurement of rock samples.

Description / Table of Contents: J. A. Crame: Origins and evolution of the Antarctic biota: an introduction / Geological Society, London, Special Publications, 47:1-8, doi:10.1144/GSL.SP.1989.047.01.01 --- L. R. M. Cocks: Antarctica’s place within Cambrian to Devonian Gondwana / Geological Society, London, Special Publications, 47:9-14, doi:10.1144/GSL.SP.1989.047.01.02 --- Françoise Debrenne and Peter D. Kruse: Cambrian Antarctic archaeocyaths / Geological Society, London, Special Publications, 47:15-28, doi:10.1144/GSL.SP.1989.047.01.03 --- Gerald F. Webers and Ellis L. Yochelson: Late Cambrian molluscan faunas and the origin of the Cephalopoda / Geological Society, London, Special Publications, 47:29-42, doi:10.1144/GSL.SP.1989.047.01.04 --- G. C. Young: The Aztec fish fauna (Devonian) of Southern Victoria Land: Evolutionary and biogeographic significance / Geological Society, London, Special Publications, 47:43-62, doi:10.1144/GSL.SP.1989.047.01.05 --- Sherri L. DeFauw: Patterns of evolution in the Dicynodontia, with special reference to austral taxa / Geological Society, London, Special Publications, 47:63-84, doi:10.1144/GSL.SP.1989.047.01.06 --- W. G. Chaloner and G. T. Creber: The phenomenon of forest growth in Antarctica: a review / Geological Society, London, Special Publications, 47:85-88, doi:10.1144/GSL.SP.1989.047.01.07 --- Mary E. Dettmann: Antarctica: Cretaceous cradle of austral temperate rainforests? / Geological Society, London, Special Publications, 47:89-105, doi:10.1144/GSL.SP.1989.047.01.08 --- Rosemary A. Askin: Endemism and heterochroneity in the Late Cretaceous (Campanian) to Paleocene palynofloras of Seymour Island, Antarctica: implications for origins, dispersal and palaeoclimates of southern floras / Geological Society, London, Special Publications, 47:107-119, doi:10.1144/GSL.SP.1989.047.01.09 --- T. H. Rich, P. V. Rich, B. Wagstaff, J. McEwen-Mason, C. B. Douthitt, and R. T. Gregory: Early Cretaceous biota from the northern side of the Australo-Antarctic rift valley / Geological Society, London, Special Publications, 47:121-130, doi:10.1144/GSL.SP.1989.047.01.10 --- R. E. Molnar: Terrestrial tetrapods in Cretaceous Antarctica / Geological Society, London, Special Publications, 47:131-140, doi:10.1144/GSL.SP.1989.047.01.11 --- G. R. Stevens: The nature and timing of biotic links between New Zealand and Antarctica in Mesozoic and early Cenozoic times / Geological Society, London, Special Publications, 47:141-166, doi:10.1144/GSL.SP.1989.047.01.12 --- Peter Doyle and Philip Howlett: Antarctic belemnite biogeography and the break-up of Gondwana / Geological Society, London, Special Publications, 47:167-182, doi:10.1144/GSL.SP.1989.047.01.13 --- Rodney M. Feldmann and Dale M. Tshudy: Evolutionary patterns in macrurous decapod crustaceans from Cretaceous to early Cenozoic rocks of the James Ross Island region, Antarctica / Geological Society, London, Special Publications, 47:183-195, doi:10.1144/GSL.SP.1989.047.01.14 --- Sankar Chatterjee and Bryan J. Small: New plesiosaurs from the Upper Cretaceous of Antarctica / Geological Society, London, Special Publications, 47:197-215, doi:10.1144/GSL.SP.1989.047.01.15 --- Judd A. Case: Antarctica: the effect of high latitude heterochroneity on the origin of the Australian marsupials / Geological Society, London, Special Publications, 47:217-226, doi:10.1144/GSL.SP.1989.047.01.16 --- K. Birkenmajer and E. Zastawniak: Late Cretaceous-early Tertiary floras of King George Island, West Antarctica: their stratigraphic distribution and palaeoclimatic significance / Geological Society, London, Special Publications, 47:227-240, doi:10.1144/GSL.SP.1989.047.01.17 --- J. T. Eastman and L. Grande: Evolution of the Antarctic fish fauna with emphasis on the Recent notothenioids / Geological Society, London, Special Publications, 47:241-252, doi:10.1144/GSL.SP.1989.047.01.18 --- Andrew Clarke and J. Alistair Crame: The origin of the Southern Ocean marine fauna / Geological Society, London, Special Publications, 47:253-268, doi:10.1144/GSL.SP.1989.047.01.19 --- R. Ewan Fordyce: Origins and evolution of Antarctic marine mammals / Geological Society, London, Special Publications, 47:269-281, doi:10.1144/GSL.SP.1989.047.01.20 --- Ellen Thomas: Development of Cenozoic deep-sea benthic foraminiferal faunas in Antarctic waters / Geological Society, London, Special Publications, 47:283-296, doi:10.1144/GSL.SP.1989.047.01.21 --- Les Watling and Michael H. Thurston: Antarctica as an evolutionary incubator: evidence from the cladistic biogeography of the amphipod Family Iphimediidae / Geological Society, London, Special Publications, 47:297-313, doi:10.1144/GSL.SP.1989.047.01.22

Description / Table of Contents: Geophysics of the Caledonian-Appalachian Orogen --- R. T. Haworth, R. Hipkin, R. D. Jacobi, M. Kane, J. P. Lefort, M. D. Max, H. G. Miller, and F. Wolff: Geophysical framework and the Appalachian-Caledonide connection / Geological Society, London, Special Publications, 38:3-20, doi:10.1144/GSL.SP.1988.038.01.01 --- F. A. Cook, D. H. Matthews, and A. W. B. Jacob: Crustal and upper mantle structure of the Appalachian-Caledonide orogen from seismic results / Geological Society, London, Special Publications, 38:21-33, doi:10.1144/GSL.SP.1988.038.01.02 --- J. C. Briden, D. V. Kent, P. L. Lapointe, J. L. Roy, R. A. Livermore, A. G. Smith, M. K. Seguin, R. Van der Voo, and D. R. Watts: Palaeomagnetic constraints on the evolution of the Caledonian-Appalachian orogen / Geological Society, London, Special Publications, 38:35-48, doi:10.1144/GSL.SP.1988.038.01.03 --- J. P. Lefort, M. D. Max, and J. Roussel: Geophysical evidence for the location of the NW boundary of Gondwanaland and its relationship with two older satellite sutures / Geological Society, London, Special Publications, 38:49-60, doi:10.1144/GSL.SP.1988.038.01.04 --- Pre-Arenig Activity in the Caledonian-Appalachian Orogen --- Derek Powell, T. B. Andersen, A. A. Drake, Jr, Leo Hall, and J. D. Keppie: The age and distribution of basement rocks in the Caledonide orogen of the N Atlantic / Geological Society, London, Special Publications, 38:63-74, doi:10.1144/GSL.SP.1988.038.01.05 --- Frederic L. Schwab, Johan P. Nystuen, and Linda Gunderson: Pre-Arenig evolution of the Appalachian-Caledonide orogen: sedimentation and stratigraphy / Geological Society, London, Special Publications, 38:75-91, doi:10.1144/GSL.SP.1988.038.01.06 --- S. Conway Morris and A. W. A. Rushton: Precambrian to Tremadoc biotas in the Caledonides / Geological Society, London, Special Publications, 38:93-109, doi:10.1144/GSL.SP.1988.038.01.07 --- Nicholas Rast, B. A. Sturt, and A. L. Harris: Early deformation in the Caledonian-Appalachian orogen / Geological Society, London, Special Publications, 38:111-122, doi:10.1144/GSL.SP.1988.038.01.08 --- Ben Harte: Lower Palaeozoic metamorphism in the Moine-Dalradian belt of the British Isles / Geological Society, London, Special Publications, 38:123-134, doi:10.1144/GSL.SP.1988.038.01.09 --- Inge Bryhni: Early Palaeozoic metamorphism in the Scandinavian Caledonides / Geological Society, London, Special Publications, 38:135-140, doi:10.1144/GSL.SP.1988.038.01.10 --- Jo Laird: Pre-Arenig metamorphism in the Appalachians / Geological Society, London, Special Publications, 38:141-147, doi:10.1144/GSL.SP.1988.038.01.11 --- D. W. Rankin, Harald Furnes, A. C. Bishop, B. Cabanis, D. J. Milton, S. J. O’Brien, and R. S. Thorpe: Plutonism and volcanism related to the pre-Arenig evolution of the Caledonide-Appalachian orogen / Geological Society, London, Special Publications, 38:149-183, doi:10.1144/GSL.SP.1988.038.01.12 --- James W. Skehan: Evolution of the Iapetus Ocean and its borders in pre-Arenig times: a synthesis / Geological Society, London, Special Publications, 38:185-229, doi:10.1144/GSL.SP.1988.038.01.13 --- Arenig-Wenlock Activity in the Caledonian-Appalachian Orogen --- R. A. Fortey and L. R. M. Cocks: Arenig to Llandovery faunal distributions in the Caledonides / Geological Society, London, Special Publications, 38:231-246, doi:10.1144/GSL.SP.1988.038.01.14 --- David L. Bruton and David A. T. Harper: Arenig-Llandovery stratigraphy and faunas across the Scandinavian Caledonides / Geological Society, London, Special Publications, 38:247-268, doi:10.1144/GSL.SP.1988.038.01.15 --- Robert B. Neuman: Palaeontological evidence bearing on the Arenig-Caradoc development of the Iapetus Ocean basin / Geological Society, London, Special Publications, 38:269-274, doi:10.1144/GSL.SP.1988.038.01.16 --- C. J. Stillman: Ordovician to Silurian volcanism in the Appalachian—Caledonian orogen / Geological Society, London, Special Publications, 38:275-290, doi:10.1144/GSL.SP.1988.038.01.17 --- Leo M. Hall and David Roberts: Timing of Ordovician deformation in the Caledonian-Appalachian orogen / Geological Society, London, Special Publications, 38:291-309, doi:10.1144/GSL.SP.1988.038.01.18 --- Jo Laird: Arenig to Wenlock age metamorphism in the Appalachians / Geological Society, London, Special Publications, 38:311-345, doi:10.1144/GSL.SP.1988.038.01.19 --- G. J. H. Oliver: Arenig to Wenlock regional metamorphism in the Paratectonic Caledonides of the British Isles: a review / Geological Society, London, Special Publications, 38:347-363, doi:10.1144/GSL.SP.1988.038.01.20 --- R. D. Dallmeyer: Polyphase tectonothermal evolution of the Scandinavian Caledonides / Geological Society, London, Special Publications, 38:365-379, doi:10.1144/GSL.SP.1988.038.01.21 --- David R. Wones and A. K. Sinha: A brief review of early Ordovician to Devonian plutonism in the N American Caledonides / Geological Society, London, Special Publications, 38:381-388, doi:10.1144/GSL.SP.1988.038.01.22 --- W. E. Stephens: Granitoid plutonism in the Caledonian orogen of Europe / Geological Society, London, Special Publications, 38:389-403, doi:10.1144/GSL.SP.1988.038.01.23 --- W. S. McKerrow: The development of the Iapetus Ocean from the Arenig to the Wenlock / Geological Society, London, Special Publications, 38:405-412, doi:10.1144/GSL.SP.1988.038.01.24 --- Wenlock to Mid-Devonian Activity in the Caledonian-Appalachian Orogen --- M. F. Thirlwall: Wenlock to mid-Devonian volcanism of the Caledonian-Appalachian orogen / Geological Society, London, Special Publications, 38:415-428, doi:10.1144/GSL.SP.1988.038.01.25 --- David Roberts: Timing of Silurian to middle Devonian deformation in the Caledonides of Scandinavia, Svalbard and E Greenland / Geological Society, London, Special Publications, 38:429-435, doi:10.1144/GSL.SP.1988.038.01.26 --- W.S. McKerrow: Wenlock to Givetian deformation in the British Isles and the Canadian Appalachians / Geological Society, London, Special Publications, 38:437-448, doi:10.1144/GSL.SP.1988.038.01.27 --- P. H. Osberg: Silurian to Lower Carboniferous tectonism in the Appalachians of the USA / Geological Society, London, Special Publications, 38:449-452, doi:10.1144/GSL.SP.1988.038.01.28 --- Peter Robinson, R. J. Tracy, D. S. Santallier, P.-G. Andreasson, and J. I. Gil-Ibarguchi: Scandian-Acadian-Caledonian sensu strictu metamorphism in the age range 430–360 Ma / Geological Society, London, Special Publications, 38:453-467, doi:10.1144/GSL.SP.1988.038.01.29 --- D. V. Kent and J. D. Keppie: Silurian-Permian palaeocontinental reconstructions and circum-Atlantic tectonics / Geological Society, London, Special Publications, 38:469-480, doi:10.1144/GSL.SP.1988.038.01.30 --- N. J. Soper: Timing and geometry of collision, terrane accretion and sinistral strike-slip events in the British Caledonides / Geological Society, London, Special Publications, 38:481-492, doi:10.1144/GSL.SP.1988.038.01.31 --- J. Chaloupský: Caledonian folding in the Bohemian Massif / Geological Society, London, Special Publications, 38:493-498, doi:10.1144/GSL.SP.1988.038.01.32 --- Robert D. Hatcher, Jr: The third synthesis: Wenlock to mid-Devonian (end of Acadian orogeny) / Geological Society, London, Special Publications, 38:499-504, doi:10.1144/GSL.SP.1988.038.01.33 --- Mid-Devonian-Permian Activity in the Caledonian-Appalachian Orogen --- Robert D. Hatcher, Jr: Basement-cover relationships in the Appalachian-Caledonian-Variscan orogen: mid-Devonian (end of Acadian orogeny) to end of Permian / Geological Society, London, Special Publications, 38:507-514, doi:10.1144/GSL.SP.1988.038.01.34 --- William A. Thomas and Paul E. Schenk: Late Palaeozoic sedimentation along the Appalachian orogen / Geological Society, London, Special Publications, 38:515-530, doi:10.1144/GSL.SP.1988.038.01.35 --- K. C. Allen and D. L. Dineley: Mid-Devonian to mid-Permian floral and faunal regions and provinces / Geological Society, London, Special Publications, 38:531-548, doi:10.1144/GSL.SP.1988.038.01.36 --- Michael Robert Leeder: Devono-Carboniferous river systems and sediment dispersal from the orogenic belts and cratons of NW Europe / Geological Society, London, Special Publications, 38:549-558, doi:10.1144/GSL.SP.1988.038.01.37 --- O. Don Hermes and Daniel P. Murray: Middle Devonian to Permian plutonism and volcanism in the N American Appalachians / Geological Society, London, Special Publications, 38:559-571, doi:10.1144/GSL.SP.1988.038.01.38 --- E. H. Francis: Mid-Devonian to early Permian volcanism: Old World / Geological Society, London, Special Publications, 38:573-584, doi:10.1144/GSL.SP.1988.038.01.39 --- Nicholas Rast: Tectonic implications of the timing of the Variscan orogeny / Geological Society, London, Special Publications, 38:585-595, doi:10.1144/GSL.SP.1988.038.01.40 --- Daniel P. Murray: Post-Acadian metamorphism in the Appalachians / Geological Society, London, Special Publications, 38:597-609, doi:10.1144/GSL.SP.1988.038.01.41 --- Francisco J. Martínez and Joël Rolet: Late Palaeozoic metamorphism in the northwestern Iberian Peninsula, Brittany and related areas in SW Europe / Geological Society, London, Special Publications, 38:611-620, doi:10.1144/GSL.SP.1988.038.01.42 --- John Rodgers: Fourth time-slice: mid-Devonian to Permian synthesis / Geological Society, London, Special Publications, 38:621-626, doi:10.1144/GSL.SP.1988.038.01.43

Description / Table of Contents: M. G. Audley-Charles and A. Hallam: Introduction / Geological Society, London, Special Publications, 37:1-4, doi:10.1144/GSL.SP.1988.037.01.01 --- Neville J. Price, Geoffrey D. Price, and Sarah L. Price: Gravity glide and plate tectonics / Geological Society, London, Special Publications, 37:5-21, doi:10.1144/GSL.SP.1988.037.01.02 --- J. F. Dewey: Lithospheric stress, deformation, and tectonic cycles: the disruption of Pangaea and the closure of Tethys / Geological Society, London, Special Publications, 37:23-40, doi:10.1144/GSL.SP.1988.037.01.03 --- Robert Hall: Basement and cover rock history in western Tethys: HT-LP metamorphism associated with extensional rifting of Gondwana / Geological Society, London, Special Publications, 37:41-50, doi:10.1144/GSL.SP.1988.037.01.04 --- C. D. Mann and C. Vita-Finzi: Holocene serial folding in the Zagros / Geological Society, London, Special Publications, 37:51-59, doi:10.1144/GSL.SP.1988.037.01.05 --- D. H. Tarling: Gondwanaland and the evolution of the Indian Ocean / Geological Society, London, Special Publications, 37:61-77, doi:10.1144/GSL.SP.1988.037.01.06 --- M. G. Audley-Charles: Evolution of the southern margin of Tethys (North Australian region) from early Permian to late Cretaceous / Geological Society, London, Special Publications, 37:79-100, doi:10.1144/GSL.SP.1988.037.01.07 --- I. Metcalfe: Origin and assembly of south-east Asian continental terranes / Geological Society, London, Special Publications, 37:101-118, doi:10.1144/GSL.SP.1988.037.01.08 --- A. M. C. Şengör, Demir Altıner, Altan Cin, Timur Ustaömer, and K. J. Hsü: Origin and assembly of the Tethyside orogenic collage at the expense of Gondwana Land / Geological Society, London, Special Publications, 37:119-181, doi:10.1144/GSL.SP.1988.037.01.09 --- L. R. M. Cocks and R. A. Fortey: Lower Palaeozoic facies and faunas around Gondwana / Geological Society, London, Special Publications, 37:183-200, doi:10.1144/GSL.SP.1988.037.01.10 --- W. G. Chaloner and G. T. Creber: Fossil plants as indicators of late Palaeozoic plate positions / Geological Society, London, Special Publications, 37:201-210, doi:10.1144/GSL.SP.1988.037.01.11 --- J. B. Waterhouse: The nature, extent, and subsequent dispersal of the Permian Tethys / Geological Society, London, Special Publications, 37:211-212, doi:10.1144/GSL.SP.1988.037.01.12 --- Edith Kristan-Tollmann: Unexpected microfaunal communities within the Triassic Tethys / Geological Society, London, Special Publications, 37:213-223, doi:10.1144/GSL.SP.1988.037.01.13 --- Jacques Thierry: Structure and palaeogeography of the western Tethys during the Jurassic: tests based on ammonite palaeobiogeography / Geological Society, London, Special Publications, 37:225-234, doi:10.1144/GSL.SP.1988.037.01.14 --- Gerd E. G. Westermann: Middle Jurassic ammonite biogeography supports ambi-Tethyan origin of Tibet / Geological Society, London, Special Publications, 37:235-239, doi:10.1144/GSL.SP.1988.037.01.15 --- Derek V. Ager: Mesozoic Turkey as part of Europe / Geological Society, London, Special Publications, 37:241-245, doi:10.1144/GSL.SP.1988.037.01.16 --- P. W. Skelton: The trans-Pacific spread of equatorial shallow-marine benthos in the Cretaceous / Geological Society, London, Special Publications, 37:247-253, doi:10.1144/GSL.SP.1988.037.01.17 --- Jean-Claude Rage: Gondwana, Tethys, and terrestrial vertebrates during the Mesozoic and Cainozoic / Geological Society, London, Special Publications, 37:255-273, doi:10.1144/GSL.SP.1988.037.01.18 --- Brian R. Rosen and Andrew B. Smith: Tectonics from fossils? Analysis of reef-coral and sea-urchin distributions from late Cretaceous to Recent, using a new method / Geological Society, London, Special Publications, 37:275-306, doi:10.1144/GSL.SP.1988.037.01.19 --- T. C. Whitmore: Phytogeography of the eastern end of Tethys / Geological Society, London, Special Publications, 37:307-311, doi:10.1144/GSL.SP.1988.037.01.20

Description / Table of Contents: J. C. Goff and B. P. J. Williams: Introduction / Geological Society, London, Special Publications, 34:NP, doi:10.1144/GSL.SP.1987.034.01.01 --- Section 1: Fluid Flow in Compacting Basins --- Richard E. Chapman: Fluid flow in sedimentary basins: a geologist’s perspective / Geological Society, London, Special Publications, 34:3-18, doi:10.1144/GSL.SP.1987.034.01.02 --- Kinji Magara: Fluid flow due to sediment loading—an application to the Arabian Gulf region / Geological Society, London, Special Publications, 34:19-28, doi:10.1144/GSL.SP.1987.034.01.03 --- Section 2: Fluid Flow in the Western Canadian Sedimentary Basin --- Brian Hitchon, S. Bachu, C. M. Sauveplane, and A. T. Lytviak: Dynamic basin analysis: an integrated approach with large data bases / Geological Society, London, Special Publications, 34:31-44, doi:10.1144/GSL.SP.1987.034.01.04 --- J. Tóth and T. Corbet: Post-Palaeocene evolution of regional groundwater flow systems and their relation to petroleum accumulations, Taber Area, southern Alberta, Canada / Geological Society, London, Special Publications, 34:45-77, doi:10.1144/GSL.SP.1987.034.01.05 --- F. W. Jones and J. A. Majorowicz: Some aspects of the thermal regime and hydrodynamics of the western Canadian sedimentary basin / Geological Society, London, Special Publications, 34:79-85, doi:10.1144/GSL.SP.1987.034.01.06 --- Harry J. Bradbury and Grant R. Woodwell: Ancient fluid flow within foreland terrains / Geological Society, London, Special Publications, 34:87-102, doi:10.1144/GSL.SP.1987.034.01.07 --- Section 3: Fluid Flow in United Kingdom Groundwater Basins --- R. A. Downing, W. M. Edmunds, and I. N. Gale: Regional groundwater flow in sedimentary basins in the U.K. / Geological Society, London, Special Publications, 34:105-125, doi:10.1144/GSL.SP.1987.034.01.08 --- A. H. Bath, A. E. Milodowski, and G. E. Strong: Fluid flow and diagenesis in the East Midlands Triassic sandstone aquifer / Geological Society, London, Special Publications, 34:127-140, doi:10.1144/GSL.SP.1987.034.01.09 --- Michael Price: Fluid flow in the Chalk of England / Geological Society, London, Special Publications, 34:141-156, doi:10.1144/GSL.SP.1987.034.01.10 --- N. P. Wilson and M. N. Luheshi: Thermal aspects of the East Midlands aquifer system / Geological Society, London, Special Publications, 34:157-169, doi:10.1144/GSL.SP.1987.034.01.11 --- Section 4: Fluid Flow in Low Permeability and Fractured Media --- J. Alexander, J. H. Black, and M. A. Brightman: The role of low-permeability rocks in regional flow / Geological Society, London, Special Publications, 34:173-183, doi:10.1144/GSL.SP.1987.034.01.12 --- J. H. Black: Flow and flow mechanisms in crystalline rock / Geological Society, London, Special Publications, 34:185-200, doi:10.1144/GSL.SP.1987.034.01.13 --- David A. Brown: The flow of water and displacement of hydrocarbons in fractured chalk reservoirs / Geological Society, London, Special Publications, 34:201-218, doi:10.1144/GSL.SP.1987.034.01.14

Description / Table of Contents: Jim Marshall: Diagenesis and Sedimentary Sequences—Introduction / Geological Society, London, Special Publications, 36:v-vi, doi:10.1144/GSL.SP.1987.036.01.01: Diagenetic Processes --- Ian R. Goldsmith and Peter King: Hydrodynamic modelling of cementation patterns in modern reefs / Geological Society, London, Special Publications, 36:1-13, doi:10.1144/GSL.SP.1987.036.01.02 --- H. G. Machel: Some aspects of diagenetic sulphate-hydrocarbon redox reactions / Geological Society, London, Special Publications, 36:15-28, doi:10.1144/GSL.SP.1987.036.01.03 --- S. N. Palmer and M. E. Barton: Porosity reduction, microfabric and resultant lithification in UK uncemented sands / Geological Society, London, Special Publications, 36:29-40, doi:10.1144/GSL.SP.1987.036.01.04 --- R. Raiswell: Non-steady state microbiological diagenesis and the origin of concretions and nodular limestones / Geological Society, London, Special Publications, 36:41-54, doi:10.1144/GSL.SP.1987.036.01.05 --- E. A. Warren: The application of a solution-mineral equilibrium model to the diagenesis of Carboniferous sandstones, Bothamsall oilfield, East Midlands, England / Geological Society, London, Special Publications, 36:55-69, doi:10.1144/GSL.SP.1987.036.01.06 --- Early Diagenesis --- T. R. Astin: Petrology (including fluorescence microscopy) of cherts from the Portlandian of Wiltshire, UK—evidence of an episode of meteoric water circulation / Geological Society, London, Special Publications, 36:73-85, doi:10.1144/GSL.SP.1987.036.01.07 --- Greg A. Carson: Silicification fabrics from the Cenomanian and basal Turonian of Devon, England: isotopic results / Geological Society, London, Special Publications, 36:87-102, doi:10.1144/GSL.SP.1987.036.01.08 --- J. D. Kantorowicz, I. D. Bryant, and J. M. Dawans: Controls on the geometry and distribution of carbonate cements in Jurassic sandstones: Bridport Sands, southern England and Viking Group, Troll Field, Norway / Geological Society, London, Special Publications, 36:103-118, doi:10.1144/GSL.SP.1987.036.01.09 --- J. J. Pueyo Mur and M. Inglés Urpinell: Magnesite formation in recent playa lakes, Los Monegros, Spain / Geological Society, London, Special Publications, 36:119-122, doi:10.1144/GSL.SP.1987.036.01.10 --- C. Taberner and C. Santisteban: Mixed-water dolomitization in a transgressive beach-ridge system, Eocene Catalan Basin, NE Spain / Geological Society, London, Special Publications, 36:123-139, doi:10.1144/GSL.SP.1987.036.01.11 --- R. D. A. Smith: Early diagenetic phosphate cements in a turbidite basin / Geological Society, London, Special Publications, 36:141-156, doi:10.1144/GSL.SP.1987.036.01.12 --- Zhao Xun and Ian J. Fairchild: Mixing zone dolomitization of Devonian carbonates, Guangxi, South China / Geological Society, London, Special Publications, 36:157-170, doi:10.1144/GSL.SP.1987.036.01.13 --- Regional Studies and Burial Diagenesis --- A. H. Bath, A. E. Milodowski, and B. Spiro: Diagenesis of carbonate cements in Permo-Triassic sandstones in the Wessex and East Yorkshire-Lincolnshire Basins, UK: a stable isotope study / Geological Society, London, Special Publications, 36:173-190, doi:10.1144/GSL.SP.1987.036.01.14 --- J. R. Boles: Six million year diagenetic history, North Coles Levee, San Joaquin Basin, California / Geological Society, London, Special Publications, 36:191-200, doi:10.1144/GSL.SP.1987.036.01.15 --- D. Emery: Trace-element source and mobility during limestone burial diagenesis—an example from the Middle Jurassic of eastern England / Geological Society, London, Special Publications, 36:201-217, doi:10.1144/GSL.SP.1987.036.01.16 --- Lynton S. Land and R. Stephen Fisher: Wilcox sandstone diagenesis, Texas Gulf Coast: a regional isotopic comparison with the Frio Formation / Geological Society, London, Special Publications, 36:219-235, doi:10.1144/GSL.SP.1987.036.01.17 --- David C. Harris and William J. Meyers: Regional dolomitization of subtidal shelf carbonates: Burlington and Keokuk Formations (Mississippian), Iowa and Illinois / Geological Society, London, Special Publications, 36:237-258, doi:10.1144/GSL.SP.1987.036.01.18 --- J. D. Hudson and J. E. Andrews: The diagenesis of the Great Estuarine Group, Middle Jurassic, Inner Hebrides, Scotland / Geological Society, London, Special Publications, 36:259-276, doi:10.1144/GSL.SP.1987.036.01.19 --- Fred J. Longstaffe and Avner Ayalon: Oxygen-isotope studies of clastic diagenesis in the Lower Cretaceous Viking Formation, Alberta: implications for the role of meteoric water / Geological Society, London, Special Publications, 36:277-296, doi:10.1144/GSL.SP.1987.036.01.20 --- J. Parnell: Secondary porosity in hydrocarbon-bearing transgressive sandstones on an unstable Lower Palaeozoic continental shelf, Welsh Borderland / Geological Society, London, Special Publications, 36:297-312, doi:10.1144/GSL.SP.1987.036.01.21 --- G. C. Saigal and K. Bjørlykke: Carbonate cements in clastic reservoir rocks from offshore Norway—relationships between isotopic composition, textural development and burial depth / Geological Society, London, Special Publications, 36:313-324, doi:10.1144/GSL.SP.1987.036.01.22 --- G. E. Strong and A. E. Milodowski: Aspects of the diagenesis of the Sherwood Sandstones of the Wessex Basin and their influence on reservoir characteristics / Geological Society, London, Special Publications, 36:325-337, doi:10.1144/GSL.SP.1987.036.01.23 --- C. B. de Wet: Deposition and diagenesis in an extensional basin: the Corallian Formation (Jurassic) near Oxford, England / Geological Society, London, Special Publications, 36:339-353, doi:10.1144/GSL.SP.1987.036.01.24

Description / Table of Contents: Mike Coward and Dorothee Dietrich: Alpine tectonics — an overview / Geological Society, London, Special Publications, 45:1-29, doi:10.1144/GSL.SP.1989.045.01.01 --- Tectonic Evolution of the External Zones of the Alps --- J. G. Ramsay: Fold and fault geometry in the western Helvetic nappes of Switzerland and France and its implication for the evolution of the arc of the western Alps / Geological Society, London, Special Publications, 45:33-45, doi:10.1144/GSL.SP.1989.045.01.02 --- D. Dietrich and M. Casey: A new tectonic model for the Helvetic nappes / Geological Society, London, Special Publications, 45:47-63, doi:10.1144/GSL.SP.1989.045.01.03 --- J.-P. Gratier, G. Ménard, and R. Arpin: Strain-displacement compatibility and restoration of the Chaînes Subalpines of the western Alps / Geological Society, London, Special Publications, 45:65-81, doi:10.1144/GSL.SP.1989.045.01.04 --- N. Fry: Southwestward thrusting and tectonics of the western Alps / Geological Society, London, Special Publications, 45:83-109, doi:10.1144/GSL.SP.1989.045.01.05 --- Tectonic Evolution of the Internal and Southern Zones of the Alps --- O. Merle, P. R. Cobbold, and S. Schmid: Tertiary kinematics in the Lepontine dome / Geological Society, London, Special Publications, 45:113-134, doi:10.1144/GSL.SP.1989.045.01.06 --- J. P. Platt, P. C. Cunningham, P. Weston, G. S. Lister, F. Peel, T. Baudin, and H. Dondey: Thrusting and backthrusting in the Briançonnais domain of the western Alps / Geological Society, London, Special Publications, 45:135-152, doi:10.1144/GSL.SP.1989.045.01.07 --- S. M. Schmid, H. R. Aebli, F. Heller, and A. Zingg: The role of the Periadriatic Line in the tectonic evolution of the Alps / Geological Society, London, Special Publications, 45:153-171, doi:10.1144/GSL.SP.1989.045.01.08 --- A. C. Ellis, A. C. Barnicoat, and N. Fry: Structural and metamorphic constraints on the tectonic evolution of the upper Pennine Alps / Geological Society, London, Special Publications, 45:173-188, doi:10.1144/GSL.SP.1989.045.01.09 --- J. Ridley: Structural and metamorphic history of a segment of the Sesia-Lanzo zone, and its bearing on the kinematics of Alpine deformation in the western Alps / Geological Society, London, Special Publications, 45:189-201, doi:10.1144/GSL.SP.1989.045.01.10 --- K. H. Brodie, E. H. Rutter, and D. Rex: On the age of deep crustal extensional faulting in the Ivrea zone, northern Italy / Geological Society, London, Special Publications, 45:203-210, doi:10.1144/GSL.SP.1989.045.01.11 --- D. Roeder: South-Alpine thrusting and trans-Alpine convergence / Geological Society, London, Special Publications, 45:211-227, doi:10.1144/GSL.SP.1989.045.01.12 --- H. P. Laubscher: The tectonics of the southern Alps and the Austro-Alpine nappes: a comparison / Geological Society, London, Special Publications, 45:229-241, doi:10.1144/GSL.SP.1989.045.01.13 --- L. Ratschbacher and F. Neubauer: West-directed décollement of Austro-Alpine cover nappes in the eastern Alps: geometrical and rheological considerations / Geological Society, London, Special Publications, 45:243-262, doi:10.1144/GSL.SP.1989.045.01.14 --- Models of the Development of the Alpine Chain --- J. F. Dewey, M. L. Helman, S. D. Knott, E. Turco, and D. H. W. Hutton: Kinematics of the western Mediterranean / Geological Society, London, Special Publications, 45:265-283, doi:10.1144/GSL.SP.1989.045.01.15 --- J. E. T. Channell and J. C. Mareschal: Delamination and asymmetric lithospheric thickening in the development of the Tyrrhenian Rift / Geological Society, London, Special Publications, 45:285-302, doi:10.1144/GSL.SP.1989.045.01.16 --- St. Mueller: Deep-reaching geodynamic processes in the Alps / Geological Society, London, Special Publications, 45:303-328, doi:10.1144/GSL.SP.1989.045.01.17 --- P. Vialon, P. Rochette, and G. Ménard: Indentation and rotation in the western Alpine arc / Geological Society, London, Special Publications, 45:329-338, doi:10.1144/GSL.SP.1989.045.01.18 --- R. Lacassin: Plate-scale kinematics and compatibility of crustal shear zones in the Alps / Geological Society, London, Special Publications, 45:339-352, doi:10.1144/GSL.SP.1989.045.01.19 --- J. C. Hunziker, J. Desmons, and G. Martinotti: Alpine thermal evolution in the central and the western Alps / Geological Society, London, Special Publications, 45:353-367, doi:10.1144/GSL.SP.1989.045.01.20 --- A. J. Hurford, M. Flisch, and E. Jäger: Unravelling the thermo-tectonic evolution of the Alps: a contribution from fission track analysis and mica dating / Geological Society, London, Special Publications, 45:369-398, doi:10.1144/GSL.SP.1989.045.01.21 --- F. Heller, W. Lowrie, and A. M. Hirt: A review of palaeomagnetic and magnetic anisotropy results from the Alps / Geological Society, London, Special Publications, 45:399-420, doi:10.1144/GSL.SP.1989.045.01.22 --- K. J. Hsü: Time and place in Alpine orogenesis — the Fermor Lecture / Geological Society, London, Special Publications, 45:421-443, doi:10.1144/GSL.SP.1989.045.01.23

Description / Table of Contents: M. A. Cooper and G. D. Williams: Introduction / Geological Society, London, Special Publications, 44:vii, doi:10.1144/GSL.SP.1989.044.01.01 --- Modelling and Theoretical Concepts --- G. D. Williams, C. M. Powell, and M. A. Cooper: Geometry and kinematics of inversion tectonics / Geological Society, London, Special Publications, 44:3-15, doi:10.1144/GSL.SP.1989.044.01.02 --- A. B. Hayward and R. H. Graham: Some geometrical characteristics of inversion / Geological Society, London, Special Publications, 44:17-39, doi:10.1144/GSL.SP.1989.044.01.03 --- K. R. McClay: Analogue models of inversion tectonics / Geological Society, London, Special Publications, 44:41-59, doi:10.1144/GSL.SP.1989.044.01.04 --- Inversion in the Alps and Alpine Foreland --- P. A. Ziegler: Geodynamic model for Alpine intra-plate compressional deformation in Western and Central Europe / Geological Society, London, Special Publications, 44:63-85, doi:10.1144/GSL.SP.1989.044.01.05 --- P. C. de Graciansky, G. Dardeau, M. Lemoine, and P. Tricart: The inverted margin of the French Alps and foreland basin inversion / Geological Society, London, Special Publications, 44:87-104, doi:10.1144/GSL.SP.1989.044.01.06 --- R. W. H. Butler: The influence of pre-existing basin structure on thrust system evolution in the Western Alps / Geological Society, London, Special Publications, 44:105-122, doi:10.1144/GSL.SP.1989.044.01.07 --- I. R. Simpson, M. Gravestock, D. Ham, H. Leach, and S. D. Thompson: Notes and cross-sections illustrating inversion tectonics in the Wessex Basin / Geological Society, London, Special Publications, 44:123-129, doi:10.1144/GSL.SP.1989.044.01.08 --- D. G. Roberts: Basin inversion in and around the British Isles / Geological Society, London, Special Publications, 44:131-150, doi:10.1144/GSL.SP.1989.044.01.09 --- Inversion on the European Continental Shelf --- J. A. Cartwright: The kinematics of inversion in the Danish Central Graben / Geological Society, London, Special Publications, 44:153-175, doi:10.1144/GSL.SP.1989.044.01.10 --- T. J. Chapman: The Permian to Cretaceous structural evolution of the Western Approaches Basin (Melville sub-basin), UK / Geological Society, London, Special Publications, 44:177-200, doi:10.1144/GSL.SP.1989.044.01.11 --- M. E. Badley, J. D. Price, and L. C. Backshall: Inversion, reactivated faults and related structures: seismic examples from the southern North Sea / Geological Society, London, Special Publications, 44:201-219, doi:10.1144/GSL.SP.1989.044.01.12 --- Inversion in Other Geological Environments --- C. M. Powell and G. D. Williams: The Lewis Thrust/Rocky Mountain trench fault system in Northwest Montana, USA: an example of negative inversion tectonics? / Geological Society, London, Special Publications, 44:223-234, doi:10.1144/GSL.SP.1989.044.01.13 --- K. R. McClay, M. W. Insley, and R. Anderton: Inversion of the Kechika Trough, Northeastern British Columbia, Canada / Geological Society, London, Special Publications, 44:235-257, doi:10.1144/GSL.SP.1989.044.01.14 --- C. K. Morley: Basin inversion in the Osen-Røa thrust sheet, Southern Norway / Geological Society, London, Special Publications, 44:259-273, doi:10.1144/GSL.SP.1989.044.01.15 --- M. P. Coward, M. A. Enfield, and M. W. Fischer: Devonian basins of Northern Scotland: extension and inversion related to Late Caledonian — Variscan tectonics / Geological Society, London, Special Publications, 44:275-308, doi:10.1144/GSL.SP.1989.044.01.16 --- M. C. Daly, J. Chorowicz, and J. D. Fairhead: Rift basin evolution in Africa: the influence of reactivated steep basement shear zones / Geological Society, London, Special Publications, 44:309-334, doi:10.1144/GSL.SP.1989.044.01.17 --- M. A. Cooper, G. D. Williams, P. C. de Graciansky, R. W. Murphy, T. Needham, D. de Paor, R. Stoneley, S. P. Todd, J. P. Turner, and P. A. Ziegler: Inversion tectonics — a discussion / Geological Society, London, Special Publications, 44:335-347, doi:10.1144/GSL.SP.1989.044.01.18 --- Abstracts --- I. W. D. Dalziel: Inversion of circum-Pacific marginal basins / Geological Society, London, Special Publications, 44:351, doi:10.1144/GSL.SP.1989.044.01.19 --- J. F. Dewey: Kinematics and dynamics of basin inversion / Geological Society, London, Special Publications, 44:352, doi:10.1144/GSL.SP.1989.044.01.20 --- A. Gibbs and A. Beach: Extensional tectonics in a convergent intra-plate setting: linked inversions on oblique and frontal ramps / Geological Society, London, Special Publications, 44:353, doi:10.1144/GSL.SP.1989.044.01.21 --- R. Gillcrist, M. P. Coward, B. Trudgill, A. Pecher, and J. L. Mugnier: Structural inversion in the external French Alps / Geological Society, London, Special Publications, 44:354, doi:10.1144/GSL.SP.1989.044.01.22 --- N. J. Kusznir and G. D. Williams: Geometric, thermal and isostatic constraints on basin inversion / Geological Society, London, Special Publications, 44:355, doi:10.1144/GSL.SP.1989.044.01.23 --- B. van Hoorn: Structural evolution, timing and tectonic style of the Sole Pit inversion / Geological Society, London, Special Publications, 44:356, doi:10.1144/GSL.SP.1989.044.01.24

Description / Table of Contents: A. D. Saunders and M. J. Norry: Introduction / Geological Society, London, Special Publications, 42:vii-viii, doi:10.1144/GSL.SP.1989.042.01.01 --- I. G. Gass: Magmatic processes at and near constructive plate margins as deduced from the Troodos (Cyprus) and Semail Nappe (N Oman) ophiolites / Geological Society, London, Special Publications, 42:1-15, doi:10.1144/GSL.SP.1989.042.01.02 --- Robert S. White: Asthenospheric control on magmatism in the ocean basins / Geological Society, London, Special Publications, 42:17-27, doi:10.1144/GSL.SP.1989.042.01.03 --- John G. Spray: Upper mantle segregation processes: evidence from alpine-type peridotites / Geological Society, London, Special Publications, 42:29-40, doi:10.1144/GSL.SP.1989.042.01.04 --- James H. Natland: Partial melting of a lithologically heterogeneous mantle: inferences from crystallization histories of magnesian abyssal tholeiites from the Siqueiros Fracture Zone / Geological Society, London, Special Publications, 42:41-70, doi:10.1144/GSL.SP.1989.042.01.05 --- H. J. B. Dick: Abyssal peridotites, very slow spreading ridges and ocean ridge magmatism / Geological Society, London, Special Publications, 42:71-105, doi:10.1144/GSL.SP.1989.042.01.06 --- Sherman H. Bloomer, James H. Natland, and Robert L. Fisher: Mineral relationships in gabbroic rocks from fracture zones of Indian Ocean ridges: evidence for extensive fractionation, parental diversity and boundary-layer recrystallization / Geological Society, London, Special Publications, 42:107-124, doi:10.1144/GSL.SP.1989.042.01.07 --- Don Elthon: Pressure of origin of primary mid-ocean ridge basalts / Geological Society, London, Special Publications, 42:125-136, doi:10.1144/GSL.SP.1989.042.01.08 --- Toshitsugu Fujii: Genesis of mid-ocean ridge basalts / Geological Society, London, Special Publications, 42:137-146, doi:10.1144/GSL.SP.1989.042.01.09 --- Z. A. Palacz and J. A. Wolff: Strontium, neodymium and lead isotope characteristics of the Granadilla Pumice, Tenerife: a study of the causes of strontium isotope disequilibrium in felsic pyroclastic deposits / Geological Society, London, Special Publications, 42:147-159, doi:10.1144/GSL.SP.1989.042.01.10 --- M. Storey, J. A. Wolff, M. J. Norry, and G. F. Marriner: Origin of hybrid lavas from Agua de Pau volcano, Sao Miguel, Azores / Geological Society, London, Special Publications, 42:161-180, doi:10.1144/GSL.SP.1989.042.01.11 --- G. Thompson, W. B. Bryan, and S. E. Humphris: Axial volcanism on the East Pacific Rise, 10–12°N / Geological Society, London, Special Publications, 42:181-200, doi:10.1144/GSL.SP.1989.042.01.12 --- Johann Helgason: The Fjallgardar volcanic ridge in NE Iceland: an aborted early stage plate boundary or a volcanically dormant zone? / Geological Society, London, Special Publications, 42:201-213, doi:10.1144/GSL.SP.1989.042.01.13 --- P. A. Floyd: Geochemical features of intraplate oceanic plateau basalts / Geological Society, London, Special Publications, 42:215-230, doi:10.1144/GSL.SP.1989.042.01.14 --- G. R. Davies, R. A. Cliff, M. J. Norry, and D. C. Gerlach: A combined chemical and Pb-Sr-Nd isotope study of the Azores and Cape Verde hot-spots: the geodynamic implications / Geological Society, London, Special Publications, 42:231-255, doi:10.1144/GSL.SP.1989.042.01.15 --- D. J. Chaffey, R. A. Cliff, and B. M. Wilson: Characterization of the St Helena magma source / Geological Society, London, Special Publications, 42:257-276, doi:10.1144/GSL.SP.1989.042.01.16 --- J.-L. Joron and M. Treuil: Hygromagmaphile element distributions in oceanic basalts as fingerprints of partial melting and mantle heterogeneities: a specific approach and proposal of an identification and modelling method / Geological Society, London, Special Publications, 42:277-299, doi:10.1144/GSL.SP.1989.042.01.17 --- D. E. Fisher: Evaluation of rare gas data in relation to oceanic magmas / Geological Society, London, Special Publications, 42:301-311, doi:10.1144/GSL.SP.1989.042.01.18 --- S.-s. Sun and W. F. McDonough: Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes / Geological Society, London, Special Publications, 42:313-345, doi:10.1144/GSL.SP.1989.042.01.19 --- B. J. Murton: Tectonic controls on boninite genesis / Geological Society, London, Special Publications, 42:347-377, doi:10.1144/GSL.SP.1989.042.01.20

Description / Table of Contents: J.S. Daly, R.A. Cliff, and B.W.D. Yardley: Preface / Geological Society, London, Special Publications, 43:vii-viii, doi:10.1144/GSL.SP.1989.043.01.01 --- E. J. Essene: The current status of thermobarometry in metamorphic rocks / Geological Society, London, Special Publications, 43:1-44, doi:10.1144/GSL.SP.1989.043.01.02 --- L. Ya. Aranovich and K. K. Podlesskii: Geothermobarometry of high-grade metapelites: simultaneously operating reactions / Geological Society, London, Special Publications, 43:45-61, doi:10.1144/GSL.SP.1989.043.01.03 --- Frank S. Spear: Relative thermobarometry and metamorphic P-T, paths / Geological Society, London, Special Publications, 43:63-81, doi:10.1144/GSL.SP.1989.043.01.04 --- R. H. Vernon: Porphyroblast-matrix microstructural relationships: recent approaches and problems / Geological Society, London, Special Publications, 43:83-102, doi:10.1144/GSL.SP.1989.043.01.05 --- John Ridley: Vertical movement in orogenic belts and the timing of metamorphism relative to deformation / Geological Society, London, Special Publications, 43:103-115, doi:10.1144/GSL.SP.1989.043.01.06 --- R. A. Jamieson and C. Beaumont: Deformation and metamorphism in convergent orogens: a model for uplift and exhumation of metamorphic terrains / Geological Society, London, Special Publications, 43:117-129, doi:10.1144/GSL.SP.1989.043.01.07 --- Peter K. Zeitler: The geochronology of metamorphic processes / Geological Society, London, Special Publications, 43:131-147, doi:10.1144/GSL.SP.1989.043.01.08 --- James J. Irwin, Charles Kirschbaum, Tek. H. Lim, Derek Powell, and William E. Glassley: A laser-microprobe study of argon isotopes in deformed pegmatites from the Northern Highlands of Scotland / Geological Society, London, Special Publications, 43:149-160, doi:10.1144/GSL.SP.1989.043.01.09 --- A. Reuter and R. D. Dallmeyer: K-Ar and 40Ar/39Ar dating of cleavage formed during very low-grade metamorphism: a review / Geological Society, London, Special Publications, 43:161-171, doi:10.1144/GSL.SP.1989.043.01.10 --- Hanan J. Kisch: Discordant relationship between degree of very low-grade metamorphism and the development of slaty cleavage / Geological Society, London, Special Publications, 43:173-185, doi:10.1144/GSL.SP.1989.043.01.11 --- J. J. De Yoreo, D. R. Lux, and C. V. Guidotti: The role of crustal anatexis and magma migration in the thermal evolution of regions of thickened continental crust / Geological Society, London, Special Publications, 43:187-202, doi:10.1144/GSL.SP.1989.043.01.12 --- C. P. Chamberlain and Douglas Rumble III: The influence of fluids on the thermal history of a metamorphic terrain: New Hampshire, USA / Geological Society, London, Special Publications, 43:203-213, doi:10.1144/GSL.SP.1989.043.01.13 --- Howard W. Day and C. Page Chamberlain: Implications of thermal and baric structure for controls on metamorphism: northern New England, USA / Geological Society, London, Special Publications, 43:215-222, doi:10.1144/GSL.SP.1989.043.01.14 --- L. Aguirre, B. Levi, and J. O. Nyström: The link between metamorphism, volcanism and geotectonic setting during the evolution of the Andes / Geological Society, London, Special Publications, 43:223-232, doi:10.1144/GSL.SP.1989.043.01.15 --- T. M. Gordon: Thermal evolution of the Kisseynew sedimentary gneiss belt, Manitoba: metamorphism at an early Proterozoic accretionary margin / Geological Society, London, Special Publications, 43:233-243, doi:10.1144/GSL.SP.1989.043.01.16 --- Peter H. Thompson: An empirical model for metamorphic evolution of the Archaean Slave Province and adjacent Thelon Tectonic Zone, north-western Canadian Shield / Geological Society, London, Special Publications, 43:245-263, doi:10.1144/GSL.SP.1989.043.01.17 --- Amalbikash Mukherjee: P-T-time history and thermal modelling of an anorthosite-granulite interface, Eastern Ghats metamorphic belt, India / Geological Society, London, Special Publications, 43:265-274, doi:10.1144/GSL.SP.1989.043.01.18 --- Leonid L. Perchuk: P-T-fluid regimes of metamorphism and related magmatism with specific reference to the granulite-facies Sharyzhalgay complex of Lake Baikal / Geological Society, London, Special Publications, 43:275-291, doi:10.1144/GSL.SP.1989.043.01.19 --- D. Ackermand, B. F. Windley, and A. Razafiniparany: The Precambrian mobile belt of southern Madagascar / Geological Society, London, Special Publications, 43:293-296, doi:10.1144/GSL.SP.1989.043.01.20 --- I. Cartwright and A. C. Barnicoat: Evolution of the Scourian complex / Geological Society, London, Special Publications, 43:297-301, doi:10.1144/GSL.SP.1989.043.01.21 --- M. A. H. Maboko, I. McDougall, and P. K. Zeitler: Metamorphic P-T path of granulites in the Musgrave Ranges, central Australia / Geological Society, London, Special Publications, 43:303-307, doi:10.1144/GSL.SP.1989.043.01.22 --- Eileen McLellan, Daniel Linder, and Jenny Thomas: Multiple granulite-facies events in the southern Appalachians, USA / Geological Society, London, Special Publications, 43:309-314, doi:10.1144/GSL.SP.1989.043.01.23 --- James M. McLelland: Pre-granulite-facies metamorphism in the Adirondack Mountains, New York / Geological Society, London, Special Publications, 43:315-317, doi:10.1144/GSL.SP.1989.043.01.24 --- F. Mengel and T. Rivers: Thermotectonic evolution of proterozoic and reworked Archaean terranes along the Nain-Churchill boundary in the Saglek Area, northern Labrador / Geological Society, London, Special Publications, 43:319-324, doi:10.1144/GSL.SP.1989.043.01.25 --- Motoyoshi Yoichi, Satoshi Matsubara, and Hiroharu Matsueda: P-T evolution of the granulite-facies rocks of the Lützow-Holm Bay region, East Antarctica / Geological Society, London, Special Publications, 43:325-329, doi:10.1144/GSL.SP.1989.043.01.26 --- H. R. Rollinson: Garnet—orthopyroxene thermobarometry of granulites from the north marginal zone of the Limpopo belt, Zimbabwe / Geological Society, London, Special Publications, 43:331-335, doi:10.1144/GSL.SP.1989.043.01.27 --- Volker Schenk: P-T-t path of the lower crust in The Hercynian fold belt of southern Calabria / Geological Society, London, Special Publications, 43:337-342, doi:10.1144/GSL.SP.1989.043.01.28 --- Daniel Vielzeuf and Christian Pin: Geodynamic implications of granulitic rocks in the Hercynian belt / Geological Society, London, Special Publications, 43:343-348, doi:10.1144/GSL.SP.1989.043.01.29 --- R. G. Warren and B. J. Hensen: The P-T evolution of the Proterozoic Arunta Block, central Australia, and Implications for tectonic evolution / Geological Society, London, Special Publications, 43:349-355, doi:10.1144/GSL.SP.1989.043.01.30 --- D. J. Waters: Metamorphic evidence for the heating and cooling path of Namaqualand granulites / Geological Society, London, Special Publications, 43:357-363, doi:10.1144/GSL.SP.1989.043.01.31 --- I. S. Buick and T. J. B. Holland: The P-T-t path associated with crustal extension, Naxos, Cyclades, Greece / Geological Society, London, Special Publications, 43:365-369, doi:10.1144/GSL.SP.1989.043.01.32 --- M. Franceschelli, I. Memmi, F. Pannuti, and C. A. Ricci: Diachronous metamorphic equilibria in the Hercynian basement of northern Sardinia, Italy / Geological Society, London, Special Publications, 43:371-375, doi:10.1144/GSL.SP.1989.043.01.33 --- P. K. Verma: The Himalayan metamorphism / Geological Society, London, Special Publications, 43:377-383, doi:10.1144/GSL.SP.1989.043.01.34 --- A. J. Barker and M. W. Anderson: The Caledonian structural—metamorphic evolution of south Troms, Norway / Geological Society, London, Special Publications, 43:385-390, doi:10.1144/GSL.SP.1989.043.01.35 --- Kevin W. Burton, Alan P. Boyle, Wendy L. Kirk, and Roger Mason: Pressure, temperature and structural evolution of the Sulitjelma fold-nappe, central Scandinavian Caledonides / Geological Society, London, Special Publications, 43:391-411, doi:10.1144/GSL.SP.1989.043.01.36 --- A. H. N. Rice, R. E. Bevins, D. Robinson, and D. Roberts: Thrust-related metamorphic inversion in the Caledonides of Finnmark, north Norway / Geological Society, London, Special Publications, 43:413-421, doi:10.1144/GSL.SP.1989.043.01.37 --- J. P. Burg, A. F. Leyreloup, F. Romney, and C. P. Delor: Inverted metamorphic zonation and Variscan thrust tectonics in the rouergue area (Massif Central, France): P-T-t record from mineral to regional scale / Geological Society, London, Special Publications, 43:423-439, doi:10.1144/GSL.SP.1989.043.01.38 --- Cl. Audren and Cl. Triboulet: Pressure–temperature–time–deformation paths in metamorphic rocks and tectonic processes, as exemplified by the Variscan orogeny in South Brittany, France / Geological Society, London, Special Publications, 43:441-446, doi:10.1144/GSL.SP.1989.043.01.39 --- David A. Brew, Arthur B. Ford, and Glen R. Himmelberg: Evolution of the western part of the Coast plutonic–metamorphic complex, South-Eastern Alaska, USA: A Summary / Geological Society, London, Special Publications, 43:447-452, doi:10.1144/GSL.SP.1989.043.01.40 --- J. C. Schumacher, Renate Schumacher, and Peter Robinson: Acadian metamorphism in central massachusetts and south-western New Hampshire: evidence for contrasting P-T trajectories / Geological Society, London, Special Publications, 43:453-460, doi:10.1144/GSL.SP.1989.043.01.41 --- Jeffrey A. Grambling, Michael L. Williams, Christopher K. Mawer, and Roger F. Smith: Metamorphic evolution of Proterozoic rocks in New Mexico / Geological Society, London, Special Publications, 43:461-467, doi:10.1144/GSL.SP.1989.043.01.42 --- G. T. R. Droop and I. Y. Al-Filali: Magmatism, deformation and high-T, low-P regional metamorphism in the Nabitah mobile belt, southern Arabian Shield / Geological Society, London, Special Publications, 43:469-480, doi:10.1144/GSL.SP.1989.043.01.43 --- Y. Hiroi and S. Kishi: P-T evolution of Abukuma metamorphic rocks in north-east Japan: metamorphic evidence for oceanic crust obduction / Geological Society, London, Special Publications, 43:481-486, doi:10.1144/GSL.SP.1989.043.01.44 --- M. Komatsu, Y. Osanai, T. Toyoshima, and S. Miyashita: Evolution of the Hidaka metamorphic belt, northern Japan / Geological Society, London, Special Publications, 43:487-493, doi:10.1144/GSL.SP.1989.043.01.45 --- Pentti Hölttä: General features of early Proterozoic metamorphism in the Pielavesi area, Near the Archaean craton Margin, central Finland / Geological Society, London, Special Publications, 43:495-499, doi:10.1144/GSL.SP.1989.043.01.46 --- Kevin A. Jones and Michael Brown: The metamorphic evolution of the Southern Brittany migmatite belt, France / Geological Society, London, Special Publications, 43:501-505, doi:10.1144/GSL.SP.1989.043.01.47 --- P. J. O'Brien: A study of retrogression in eclogites of the Oberpfalz Forest, north-east Bavaria, West Germany, and their significance in the tectonic evolution of the Bohemian Massif / Geological Society, London, Special Publications, 43:507-512, doi:10.1144/GSL.SP.1989.043.01.48 --- I. S. Sanders: Phase relations and P-T conditions for eclogite-facies rocks at Glenelg, north-west Scotland / Geological Society, London, Special Publications, 43:513-517, doi:10.1144/GSL.SP.1989.043.01.49 --- Shohei Banno and Chihiro Sakai: Geology and metamorphic evolution of the Sanbagawa metamorphic belt, Japan / Geological Society, London, Special Publications, 43:519-532, doi:10.1144/GSL.SP.1989.043.01.50 --- Akira Takasu: P-T histories of peridotite and amphibolite tectonic blocks in the Sanbagawa metamorphic belt, Japan / Geological Society, London, Special Publications, 43:533-538, doi:10.1144/GSL.SP.1989.043.01.51 --- A. C. Barnicoat and N. Fry: Eoalpine high-pressure metamorphism in the Piemonte zone of the Alps: south-west Switzerland and north-west Italy / Geological Society, London, Special Publications, 43:539-544, doi:10.1144/GSL.SP.1989.043.01.52 --- H.-J. Massonne and C. Chopin: P-T history of the Gran Paradiso (Western Alps) metagranites based on phengite geobarometry / Geological Society, London, Special Publications, 43:545-549, doi:10.1144/GSL.SP.1989.043.01.53 --- P. J. Treble: The Voltri Group, northern Italy: an Alpine ophiolite massif / Geological Society, London, Special Publications, 43:551-556, doi:10.1144/GSL.SP.1989.043.01.54 --- Colin N. Waters: The metamorphic evolution of the Schistes lustrés ophiolite, Cap Corse, Corsica / Geological Society, London, Special Publications, 43:557-562, doi:10.1144/GSL.SP.1989.043.01.55

Description / Table of Contents: Mervyn E. Jones and R. M. F. Preston: Introduction / Geological Society, London, Special Publications, 29:1-8, doi:10.1144/GSL.SP.1987.029.01.01 --- Part I: Theory and Experimental --- G. Owen: Deformation processes in unconsolidated sands / Geological Society, London, Special Publications, 29:11-24, doi:10.1144/GSL.SP.1987.029.01.02 --- J. P. Gratier: Pressure solution-deposition creep and associated tectonic differentiation in sedimentary rocks / Geological Society, London, Special Publications, 29:25-38, doi:10.1144/GSL.SP.1987.029.01.03 --- G. Mandl and R. M. Harkness: Hydrocarbon migration by hydraulic fracturing / Geological Society, London, Special Publications, 29:39-53, doi:10.1144/GSL.SP.1987.029.01.04 --- C. R. I. Clayton and M. C. Matthews: Deformation, diagenesis and the mechanical behaviour of chalk / Geological Society, London, Special Publications, 29:55-62, doi:10.1144/GSL.SP.1987.029.01.05 --- R. J. Allison: Non-destructive determination of Young’s modulus and its relationship with compressive strength, porosity and density / Geological Society, London, Special Publications, 29:63-69, doi:10.1144/GSL.SP.1987.029.01.06 --- Alex J. Maltman: A laboratory technique for investigating the deformation microstructures of water-rich sediments / Geological Society, London, Special Publications, 29:71-76, doi:10.1144/GSL.SP.1987.029.01.07 --- Alex. J. Maltman: Shear zones in argillaceous sediments—an experimental study / Geological Society, London, Special Publications, 29:77-87, doi:10.1144/GSL.SP.1987.029.01.08 --- Part II: Processes --- John R. Underhill and Nigel H. Woodcock: Faulting mechanisms in high-porosity sandstones; New Red Sandstone, Arran, Scotland / Geological Society, London, Special Publications, 29:91-105, doi:10.1144/GSL.SP.1987.029.01.09 --- Jean-Pierre Petit and Edgard Laville: Morphology and microstructures of hydroplastic slickensides in sandstone / Geological Society, London, Special Publications, 29:107-121, doi:10.1144/GSL.SP.1987.029.01.10 --- Michel Guiraud and Michel Séguret: Soft-sediment microfaulting related to compaction within the fluviodeltaic infill of the Soria strike-slip basin (northern Spain) / Geological Society, London, Special Publications, 29:123-136, doi:10.1144/GSL.SP.1987.029.01.11 --- Michael Leeder: Sediment deformation structures and the palaeotectonic analysis of sedimentary basins, with a case-study from the Carboniferous of northern England / Geological Society, London, Special Publications, 29:137-144, NP, 145-146, doi:10.1144/GSL.SP.1987.029.01.12 --- Pierre Labaume: Syn-diagenetic deformation of a turbiditic succession related to submarine gravity nappe emplacement, Autapie Nappe, French Alps / Geological Society, London, Special Publications, 29:147-163, doi:10.1144/GSL.SP.1987.029.01.13 --- S.A. Schack Pedersen: Comparative studies of gravity tectonics in Quaternary sediments and sedimentary rocks related to fold belts / Geological Society, London, Special Publications, 29:165-179, doi:10.1144/GSL.SP.1987.029.01.14 --- S. G. Farrell and S. Eaton: Slump strain in the Tertiary of Cyprus and the Spanish Pyrenees. Definition of palaeoslopes and models of soft-sediment deformation / Geological Society, London, Special Publications, 29:181-196, doi:10.1144/GSL.SP.1987.029.01.15 --- P. M. Clifford, M. C. Rice, L. L. Pryer, and F. Fueten: Mass transfer in unmetamorphosed carbonates and during low-grade metamorphism of arenites / Geological Society, London, Special Publications, 29:197-209, doi:10.1144/GSL.SP.1987.029.01.16 --- Part III: Descriptive --- K. T. Pickering: Wet-sediment deformation in the Upper Ordovician Point Leamington Formation: an active thrust-imbricate system during sedimentation, Notre Dame Bay, north-central Newfoundland / Geological Society, London, Special Publications, 29:213-218,NP,219-232,NP,234-239, doi:10.1144/GSL.SP.1987.029.01.17 --- Krzysztof Brodzikowski, Roman Gotowała, Ludwik Kasza, and Antonius J. Van Loon: The Kleszczów Graben (central Poland): reconstruction of the deformational history and inventory of the resulting soft-sediment deformational structures / Geological Society, London, Special Publications, 29:241-254, doi:10.1144/GSL.SP.1987.029.01.18 --- K. Brodzikowski, R. Gotowała, A. Hałuszczak, D. Krzyszkowski, and A. J. Van Loon: Soft-sediment deformations from glaciodeltaic, glaciolacustrine and fluviolacustrine sediments in the Kleszczów Graben (central Poland) / Geological Society, London, Special Publications, 29:255-267, doi:10.1144/GSL.SP.1987.029.01.19 --- Krzysztof Brodzikowski, Dariusz Krzyszkowski, and Antonius J. Van Loon: Endogenic processes as a cause of penecontemporaneous soft-sediment deformations in the fluviolacustrine Czyżów Series (Kleszczów Graben, central Poland) / Geological Society, London, Special Publications, 29:269-278, doi:10.1144/GSL.SP.1987.029.01.20 --- Krzysztof Brodzikowski and Andrzej Hałuszczak: Flame structures and associated deformations in Quaternary glaciolacustrine and glaciodeltaic deposits: examples from central Poland / Geological Society, London, Special Publications, 29:279-286, doi:10.1144/GSL.SP.1987.029.01.21 --- Krzysztof Brodzikowski, Andrzej Hałuszczak, Dariusz Krzyszkowski, and Antonius J. Van Loon: Genesis and diagnostic value of large-scale gravity-induced penecontemporaneous deformation horizons in Quaternary sediments of the Kleszczów Graben (central Poland) / Geological Society, London, Special Publications, 29:287-298, doi:10.1144/GSL.SP.1987.029.01.22 --- Colin A. Davenport and Philip S. Ringrose: Deformation of Scottish Quaternary sediment sequences by strong earthquake motions / Geological Society, London, Special Publications, 29:299-314, doi:10.1144/GSL.SP.1987.029.01.23 --- J. Alexander: Syn-sedimentary and burial related deformation in the Middle Jurassic non-marine formations of the Yorkshire Basin / Geological Society, London, Special Publications, 29:315-324, doi:10.1144/GSL.SP.1987.029.01.24 --- Bill Fitches: Aspects of veining in the Welsh Lower Palaeozoic Basin / Geological Society, London, Special Publications, 29:325-342, doi:10.1144/GSL.SP.1987.029.01.25

Description / Table of Contents: D. R. Bowes: Janet Watson—an appreciation and bibliography / Geological Society, London, Special Publications, 27:1-5, doi:10.1144/GSL.SP.1987.027.01.01 --- John Sutton and Janet Watson: The Lewisian complex: questions for the future / Geological Society, London, Special Publications, 27:7-11, doi:10.1144/GSL.SP.1987.027.01.02 --- R. G. Park and J. Tarney: The Lewisian complex: a typical Precambrian high-grade terrain? / Geological Society, London, Special Publications, 27:13-25, doi:10.1144/GSL.SP.1987.027.01.03 --- D. J. Fettes and J. R. Mendum: The evolution of the Lewisian complex in the Outer Hebrides / Geological Society, London, Special Publications, 27:27-44, doi:10.1144/GSL.SP.1987.027.01.04 --- J. Tarney and B. L. Weaver: Geochemistry of the Scourian complex: petrogenesis and tectonic models / Geological Society, London, Special Publications, 27:45-56, doi:10.1144/GSL.SP.1987.027.01.05 --- H. R. Rollinson and M. B. Fowler: The magmatic evolution of the Scourian complex at Gruinard Bay / Geological Society, London, Special Publications, 27:57-71, doi:10.1144/GSL.SP.1987.027.01.06 --- A. C. Barnicoat: The causes of the high-grade metamorphism of the Scourie complex, NW Scotland / Geological Society, London, Special Publications, 27:73-79, doi:10.1144/GSL.SP.1987.027.01.07 --- J. D. Sills and H. R. Rollinson: Metamorphic evolution of the mainland Lewisian complex / Geological Society, London, Special Publications, 27:81-92, doi:10.1144/GSL.SP.1987.027.01.08 --- I. Cartwright and A. C. Barnicoat: Petrology of Scourian supracrustal rocks and orthogneisses from Stoer, NW Scotland: implications for the geological evolution of the Lewisian complex / Geological Society, London, Special Publications, 27:93-107, doi:10.1144/GSL.SP.1987.027.01.09 --- N. M. S. Rock, A. E. Davis, D. Hutchison, M. Joseph, and T. K. Smith: The geochemistry of Lewisian marbles / Geological Society, London, Special Publications, 27:109-126, doi:10.1144/GSL.SP.1987.027.01.10 --- M. P. Coward and R. G. Park: The role of mid-crustal shear zones in the Early Proterozoic evolution of the Lewisian / Geological Society, London, Special Publications, 27:127-138, doi:10.1144/GSL.SP.1987.027.01.11 --- R. G. Park, A. Crane, and M. Niamatullah: Early Proterozoic structure and kinematic evolution of the southern mainland Lewisian / Geological Society, London, Special Publications, 27:139-151, doi:10.1144/GSL.SP.1987.027.01.12 --- J. Wheeler, B. F. Windley, and F. B. Davies: Internal evolution of the major Precambrian shear belt at Torridon, NW Scotland / Geological Society, London, Special Publications, 27:153-163, doi:10.1144/GSL.SP.1987.027.01.13 --- P. Attfield: The structural history of the Canisp Shear Zone / Geological Society, London, Special Publications, 27:165-173, doi:10.1144/GSL.SP.1987.027.01.14 --- S. H. White and J. Glasser: The Outer Hebrides Fault Zone: evidence for normal movements / Geological Society, London, Special Publications, 27:175-183, doi:10.1144/GSL.SP.1987.027.01.15 --- J. Hall: Physical properties of Lewisian rocks: implications for deep crustal structure / Geological Society, London, Special Publications, 27:185-192, doi:10.1144/GSL.SP.1987.027.01.16 --- D. K. Smythe: Deep seismic reflection profiling of the Lewisian foreland / Geological Society, London, Special Publications, 27:193-203, doi:10.1144/GSL.SP.1987.027.01.17 --- J. D. A. Piper: The palaeomagnetic record in the Lewisian terrain / Geological Society, London, Special Publications, 27:205-215, doi:10.1144/GSL.SP.1987.027.01.18 --- J. Tarney and B. L. Weaver: Mineralogy, petrology and geochemistry of the Scourie dykes: petrogenesis and crystallization processes in dykes intruded at depth / Geological Society, London, Special Publications, 27:217-233, doi:10.1144/GSL.SP.1987.027.01.19 --- J. S. Myers: The East Greenland Nagssugtoqidian mobile belt compared with the Lewisian complex / Geological Society, London, Special Publications, 27:235-246, doi:10.1144/GSL.SP.1987.027.01.20 --- J. Korstgård, B. Ryan, and R. Wardle: The boundary between Proterozoic and Archaean crustal blocks in central West Greenland and northern Labrador / Geological Society, London, Special Publications, 27:247-259, doi:10.1144/GSL.SP.1987.027.01.21 --- R. P. Hall, D. J. Hughes, and C. R. L. Friend: Mid-Archaean basic magmatism of southern West Greenland / Geological Society, London, Special Publications, 27:261-275, doi:10.1144/GSL.SP.1987.027.01.22 --- J. S. Myers: High-grade terrains in and around the Yilgarn Block of Western Australia / Geological Society, London, Special Publications, 27:277-284, doi:10.1144/GSL.SP.1987.027.01.23 --- S. L. Harley and L. P. Black: The Archaean geological evolution of Enderby Land, Antarctica / Geological Society, London, Special Publications, 27:285-296, doi:10.1144/GSL.SP.1987.027.01.24 --- J. D. Sills, K. Wang, Y. Yan, and B. F. Windley: The Archaean high grade gneiss terrain in E Hebei Province, NE China: geological framework and conditions of metamorphism / Geological Society, London, Special Publications, 27:297-305, doi:10.1144/GSL.SP.1987.027.01.25

Description / Table of Contents: A. J. Fleet and J. Brooks: Introduction / Geological Society, London, Special Publications, 26:1-14, doi:10.1144/GSL.SP.1987.026.01.01 --- Part I: Concepts and Methods --- J. Brooks, C. Cornford, and R. Archer: The role of hydrocarbon source rocks in petroleum exploration / Geological Society, London, Special Publications, 26:17-46, doi:10.1144/GSL.SP.1987.026.01.02 --- R. V. Tyson: The genesis and palynofacies characteristics of marine petroleum source rocks / Geological Society, London, Special Publications, 26:47-67, doi:10.1144/GSL.SP.1987.026.01.03 --- I. St. J. Fisher and J. D. Hudson: Pyrite formation in Jurassic shales of contrasting biofacies / Geological Society, London, Special Publications, 26:69-78, doi:10.1144/GSL.SP.1987.026.01.04 --- S. C. Brassell, G. Eglinton, and V. J. Howell: Palaeoenvironmental assessment of marine organic-rich sediments using molecular organic geochemistry / Geological Society, London, Special Publications, 26:79-98, doi:10.1144/GSL.SP.1987.026.01.05 --- P. A. Comet and G. Eglinton: The use of lipids as facies indicators / Geological Society, London, Special Publications, 26:99-117, doi:10.1144/GSL.SP.1987.026.01.06 --- Part II: Depositional Processes and Environments --- E. T. Degens and V. Ittekkot: The carbon cycle—tracking the path of organic particles from sea to sediment / Geological Society, London, Special Publications, 26:121-135, doi:10.1144/GSL.SP.1987.026.01.07 --- S. E. Calvert: Oceanographic controls on the accumulation of organic matter in marine sediments / Geological Society, London, Special Publications, 26:137-151, doi:10.1144/GSL.SP.1987.026.01.08 --- R. J. Morris: The formation of organic-rich deposits in two deep-water marine environments / Geological Society, London, Special Publications, 26:153-166, doi:10.1144/GSL.SP.1987.026.01.09 --- R. Pelet: A model of organic sedimentation on present-day continental margins / Geological Society, London, Special Publications, 26:167-180, doi:10.1144/GSL.SP.1987.026.01.10 --- E. Suess, L. D. Kulm, and J. S. Killingley: Coastal upwelling and a history of organic-rich mudstone deposition off Peru / Geological Society, London, Special Publications, 26:181-197, doi:10.1144/GSL.SP.1987.026.01.11 --- J. T. Parrish: Palaeo-upwelling and the distribution of organic-rich rocks / Geological Society, London, Special Publications, 26:199-205, doi:10.1144/GSL.SP.1987.026.01.12 --- J. Ferguson: The significance of carbonate ooids in petroleum source-rock studies / Geological Society, London, Special Publications, 26:207-215, doi:10.1144/GSL.SP.1987.026.01.13 --- B. R. T. Simoneit and O. E. Kawka: Hydrothermal petroleum from diatomites in the Gulf of California / Geological Society, London, Special Publications, 26:217-228, doi:10.1144/GSL.SP.1987.026.01.14 --- Part III: The Stratigraphic Record --- A. Thickpenny and J. K. Leggett: Stratigraphic distribution and palaeo-oceanographic significance of European early Palaeozoic organic-rich sediments / Geological Society, London, Special Publications, 26:231-247, doi:10.1144/GSL.SP.1987.026.01.15 --- M. J. Gibbons: The depositional environment and petroleum geochemistry of the Marl Slate-Kupferschiefer / Geological Society, London, Special Publications, 26:249, doi:10.1144/GSL.SP.1987.026.01.16 --- A. Hallam: Mesozoic marine organic-rich shales / Geological Society, London, Special Publications, 26:251-261, doi:10.1144/GSL.SP.1987.026.01.17 --- R. Stoneley: A review of petroleum source rocks in parts of the Middle East / Geological Society, London, Special Publications, 26:263-269, doi:10.1144/GSL.SP.1987.026.01.18 --- H. B. Zimmerman, A. Boersma, and F. W. McCoy: Carbonaceous sediments and palaeoenvironment of the Cretaceous South Atlantic Ocean / Geological Society, London, Special Publications, 26:271-286, doi:10.1144/GSL.SP.1987.026.01.19 --- D. A. V. Stow: South Atlantic organic-rich sediments: facies, processes and environments of deposition / Geological Society, London, Special Publications, 26:287-299, doi:10.1144/GSL.SP.1987.026.01.20 --- C. P. Summerhayes: Organic-rich Cretaceous sediments from the North Atlantic / Geological Society, London, Special Publications, 26:301-316, doi:10.1144/GSL.SP.1987.026.01.21 --- P. C. de Graciansky, E. Brosse, G. Deroo, J.-P. Herbin, C. Müller, J. Sigal, A. Schaaf, and L. Montadert: Organic-rich sediments and palaeoenvironmental reconstructions of the Cretaceous North Atlantic / Geological Society, London, Special Publications, 26:317-344, doi:10.1144/GSL.SP.1987.026.01.22 --- T. J. Bralower and H. R. Thierstein: Organic carbon and metal accumulation rates in Holocene and mid-Cretaceous sediments: palaeoceanographic significance / Geological Society, London, Special Publications, 26:345-369, doi:10.1144/GSL.SP.1987.026.01.23 --- S. O. Schlanger, M. A. Arthur, H. C. Jenkyns, and P. A. Scholle: The Cenomanian-Turonian Oceanic Anoxic Event, I. Stratigraphy and distribution of organic carbon-rich beds and the marine δ13C excursion / Geological Society, London, Special Publications, 26:371-399, doi:10.1144/GSL.SP.1987.026.01.24 --- M. A. Arthur, S. O. Schlanger, and H. C. Jenkyns: The Cenomanian-Turonian Oceanic Anoxic Event, II. Palaeoceanographic controls on organic-matter production and preservation / Geological Society, London, Special Publications, 26:401-420, doi:10.1144/GSL.SP.1987.026.01.25 --- B. M. Funnell: Anoxic non-events; alternative explanations / Geological Society, London, Special Publications, 26:421-422, doi:10.1144/GSL.SP.1987.026.01.26 --- N. J. Shackleton: The carbon isotope record of the Cenozoic: history of organic carbon burial and of oxygen in the ocean and atmosphere / Geological Society, London, Special Publications, 26:423-434, doi:10.1144/GSL.SP.1987.026.01.27

Description / Table of Contents: In a clear style, the atlas describes the origin and major characteristics of the different soil types that can be found in this environment. The atlas discusses the possible impacts of climate change on permafrost-affected soils and explains the critical role that they play in the global climate and global carbon cycles. 6. For the first time ever, the distribution of soil types for the entire northern circumpolar region can be visualised in a comprehensible manner by the lay-person. Information on the major soil types is presented in detail on twenty six map plates (the atlas has an A3 page size giving a dramatic A2 spread for maps). In a novel exercise, the World Reference Base for Soil Resources has been used as a framework for correlating knowledge from diverse national soil classification systems into a single, coherent, inter-continental product. The atlas illustrates the diversity of soil in the permafrost and seasonally frozen environments through a series of maps supported by explanatory and easily readable texts, high quality photographs and descriptive graphics. The atlas presents the reader with a series of maps that show the variation of soil properties in a circumpolar context and from a polar perspective, allowing comparisons to be made across international boundaries. In addition, larger scale maps show the distribution of major soil types by regions with descriptions of the major issues. The maps have been produced through the elaboration of harmonized soil databases for the northern circumpolar areas by Geographic Information Systems software (GIS).Through supporting texts, the atlas describes the major soil types found in northern latitudes, together with their principal properties and characteristics, the main soil forming processes, the importance of soil classification and the use of soil. Special attention is given to impact of cold climates on soil characteristics and on the relationship between climate change and soils properties (e.g. carbon dynamics, carbon sinks and sources, methane emission). In addition, the atlas illustrates how soil can be used as indicators of past climate change and present examples local and regional perspectives of the importance and functions of soil for society as a whole and particularly for indigenous northern cultures.

Description / Table of Contents: This book summarizes the results of an interdisciplinary meeting held in Obergurgl in 2006. Based on current knowledge the meeting aimed at a research strategy for the research focus “alpine space – man and environment” of Innsbruck University.

Description / Table of Contents: INTRODUCTION The evaporite deposits of the Werra district, especially in the Hattorf mining field, are considered a worldwide unique location for the occurence of numerous basalt dikes and magmatic fluid phases fixed in salt rocks. In spite of the great number of studies dealing with the magmatites in the Werra region, previous investigations have rarely attempted more than a predominantly 'qualitative' description of the basaltic rocks and the effects of volcanism on the evaporites (see Chapter 2). The method of interpreting the mineralogical and chemical composition of the evaporites at the basalt contact is based on previous works (KNIPPING 1984; KNIPPING & HERRMANN 1985). This study should contribute to understanding (i) the mechanism of intrusion of the basaltic rnelts and (ii) the metamorphic processes occurring in the evaporites caused by mobile phases during volcanism. Hence, the following methods were applied: The mineralogical and chemical description of the basaltic rocks with recent nomenclature including the possible differences between individual dikes and between surface- and subsurface-exposed basalts. Seven surface and 48 subsurface exposures at the Hattorf mine of Kali & Salz AG were studied. Application of the most recent knowledge on basalt genesis for interpreting observational and experimental results. Studies on the sulfur and carbon isotope distributions of the native sulfur from several subsurface exposures and the enrichments of gases (predominantly CO2) in the evaporites. Calculation of the spatial and temporal temperature distribution in the evaporite rocks following intrusion of the basaltic melts. For purposes of clarity a few of the terms which will be used frequently here will first be defined: basalt - all of the intrusive rocks studied can be assigned mineralogically and chemically to the basalt family in a broader sense. Thus, the terms basaltic rock or, in short, basalt will be used for these rocks. rock salt - instead of the term salt for halitic rocks the term rock salt is used. Besides, the evaporites are generally designated as host rocks (for the basalt dikes) as well. gases - especially in the German literature the term carbon dioxide or carbonic acid (= Kohlensäure) is frequently used for the gases enclosed in the evaporites of the Werra-Fulda district. ACKERMANN et al (1964) found, in addition to carbon dioxide, considerable amounts of nitrogen and minor amounts of methane. In the following therefore the terms gas mixture or gas will be used. The various basalt dikes found in the Hattorf mining field are described here in terms of their mineralogy and geochemistry for the first time. In doing so it is necessary to number them from east to west. To avoid confusion with older numerations (e.g. SIEMENS 1971) the various dike systems are designated by capital letters (A to P).

Description / Table of Contents: PREFACE This volume comprises the main lectures delivered at the Fourth International Summer School in the Mountains on "Mathematical and Numerical Techniques in Physical Geodesy", held from August 25 to September 5, 1986 in Admont, Austria. The School was organized by the Institute of Theoretical Geodesy of the Technical University Graz, Austria under the auspices of the International Association of Geodesy. All five continents were represented by 70 participants from over 20 countries. The purpose of the Summer School was to provide an introduction to advanced techniques which represent the mathematical vehicle for the treatment of modern geodetic problems, to familiarize participants with the present state of the art of global and local gravity field determination methods, ranging from orbit theory, the key satellite techniques, to inertial and standard terrestrial methods, and to discuss future scientific developments. The arrangement of this volume matches the sequence of lectures given at the School. The theoretical PART A represents the mathematical framework of modern physical geodesy, the application PART B deals with the key satellite and surface techniques, providing the detailed structure of the earth's gravity field. PART A: One of the main goals in physical geodesy, global and local gravity field determination, is pursued by extensively applying functional analytic methods. Recently special attention is being given to the base function and norm choice problem, and to the establishment of a sound link between density distributions inside the earth as the source and observed or estimated gravity field quantities as the effect. The lectures by C.C. Tscherning focus on this topic. Space and time dependent problems of discrete and continuous type are encountered in modern geodesy nowadays and dealt with in the lectures by F. Sans6. Estimation theory either in its stochastic or statistic formulation plays a key role in the processing of processes like the earth's gravity field. The consistent processing of large structured data sets calls for equally structured numerical algorithms. Spectral analysis with its powerful fast Fourier transform has become a common tool for the treatment of such problems. An introduction to spectral methods, supplemented by numerous examples, is provided by B. Hofmann-Wellenhof and H. Moritz. PART B: The theory of orbit dynamics, tailored to the near circular orbits of most geodetic satellites, is fundamental to modern geodetic satellite techniques and discussed in the lectures by O.L. Colombo. Particular emphasis is put on the interplay between orbit perturbations and the earth's disturbing gravity field and its mapping by satellite techniques like satellite altimetry, satellite-tosatellite tracking and satellite gradiometry. Satellite gradiometry, which is discussed in the lectures by R. Rummel in detail, with regard to the geometric structure of the gravitational field, the observability of the gradients, and the mathematical model underlying the gravity field recovery problem, promises to provide particularly detailed information about the gravity field of our planet. The global structure of the earth's gravity field is described in terms of earth gravity field models which are derived from both satellite and surface data. The many delicate, mathematically as well as numerically challenging problems, related to the consistent processing of very large space distributed data sets, and proposed solutions are presented in the lecture by R.H. Rapp. For many years various attempts have been made to explain the shorter wavelength part of the earth's anomalous gravity field by isostatic phenomena. Recently several high resolution topographicisostatic earth models have been computed based on global digital terrain data using different techniques fo~ the estimation of the parameters of the chosen isostatic model. A declared goal is the maximum smoothing of the observed gravity field by removing the contribution of the topography and its isostatic compensation. This topic is discussed in the lectures by H. SUnkel. Inertial methods are steadily gaining importance, power and application. This is not only due to hardware improvements in terms of precision and reliability, but also due to recent advances in the mathematical and numerical modelling of the system's performance. An investigation of the error characteristics of inertial survey systems and their interaction with the anomalous gravity field, studied in the framework of dynamic system analysis, is the topic of the lectures by K.-P. Schwarz and the key issue for further improvements and possible integrations with other positioning systems. Geodetic data have both geometric and physical ingredients of various nature. Standard geodetic processing procedures aim at a separation of geometry from physics. Integrated geodesy, in contrast, has been designed as a very sophisticated melting pot which handles practically all available geodetic data in a consistent and optimal way.lt handles surface and satellite data with either geometrically or gravity field dominated content, and geophysical data in terms of density and seismic informatlon just as well and represents as such the great synthesis of mathematical modelling in connexion with geodetic data processing techniques; these advanced ideas are presented in the lectures by G. Hein. This volume presents highlights of modern geodetic activity and takes the reader to the frontiers of current research. It is not a textbook on a closed and limited subject, but rather a reference book for graduates and scientists working in the vast and beautiful, demanding but rewarding field of earth science in general and physical geodesy in particular. The editor expresses his appreciation to all authors of this volume for their advice and help in formulating and designing the scientific program of the Summer School, for providing typewritten lecture notes, and for their excellent cooperation.

Description / Table of Contents: Biolaminated deposits, produced by microbial communities, were studied in modern peritidal environments and in the rock record. The term microbial, mat refers to modern, the term stromatolite to ancient analogs. The term biolaminated deposits was used to encompass both microbial mats and stromatolites. Microbial mat environments studied are the Gavish Sabkha, the Solar Lake, both hypersaline back-barrier systems at the Gulf of Aqaba, Sinai Peninsula, and the "Farbstreifen-Sandwatt" (versicolored sandy tidal flats) on Mellum, an island in the estuary embayment of the southern North Sea coast. Three facies-relevant categories were distinguished: (i) the mat-forming microbiota, (2) environmental conditions controlling mat types and lithology, (3) bioturbation and grazing. Cyanobacteria account for biogenic sediment accretion in all cases studied. Three major groups occur: filamentous cyanobacteria, coccoid unicells with binary fission and those with multiple fission. In the presence of these groups the following mat types evolve: (i) continuously flat (stratiform) L~-laminae (occur in all environments studied); (2) translucent, vertically extended Lv-laminae (only Gavish Sabkha and Solar Lake); (3) nodular granules (only Gavish Sabkha). Basically, the development of mats is controlled by moisture. Thus high-lying parts where the groundwater table runs more than 40 cm below surface are bare of mats. These are: The circular slope and elevated center of the Gavish Sabkha, the shorelines of the Solar Lake and the episodically flooded upper supratidal zone of Mellum Island. The following situations of water supply were found to stimulate mat growth: (i) Capillary movement of groundwater to exposed surfaces, (2) shallowest calm water, both realized in the Gavish Sabkha and the Solar Lake. On Mellum Island, mats form in the lower supratidal zone, which is flooded in the spring tide cycle and wetted during low tide by capillary groundwater. Salinity is almost that of normal seawater, whereas in the Solar Lake, it ranges from 45 °/oo to 180 °/oo and in the Gavish Sabkha, it reaches more than 300 °/oo. Salinity increase is correlated with rising concentrations of magnesium and sulfate ions. In the Gavish Sabkha, episodic sheetfloods cause high-rate sedimentation which is accidental to the living mats. Episodic low-rate sedimentation stimulates the mats to grow through the freshly deposited sediment layer. This occurs predominantly on Mellum Island due to eolian transport. Within the Gavish Sabkha, mineralogy of sediments, community structures, standing crops, redox potentials and pH are highly correlative to the increasing evenness in moisture supply which is realized by the inclination of the system below mean sea level. These conditions bring about a lateral sequence of facies types which include (I) siliciclastic biolaminites at the coastal bar base, (2) nodular to biolaminoid carbonates at saline mud flats, (3) regularly stratified stromatolitic carbonates with ooids and oncoids within the hypersaline lagoon, (4) biolaminated sulfate towardthe elevated center. High-magnesium calcite in facies type 3 precipitates around decaying organic matter and forms also the ooids and oncoids. These occur predominantly within hydroplastic Lv-laminae which provide numerous nucleation centers. Within the Solar Lake, facies type 3 (stromatolitic carbonates with ooids and oncoids) is most important, and grows to extraordinary thickness at the lake's shelf. The regular alternation of dark and light laminae results from seasonally oscillating water depths. These conditions couple back over changing light and salinity intensities to changing dominance structures of mat-building communities. Increasing salinity correlates with decreasing water depth and accounts for the relative abundance of coccoid unicells and diatoms, both active producers of extracellular slimes (Lv-laminae). Water depths locally or temporarily increased favor surface colonization by Mic~ocoleu8 chthonoplastes (Lh-laminae). The biolaminated deposits of the versicolored tidal flats on Mellum Island are similar to facies type 1 of the Gavish Sabkha (siliciclastic biolaminites). Differences exist in the lithology: Sediments upon or through which the mats on Mellum Island grow are made up of clean sand. The grains originate predominantly from re-worked glacial sediments and are rounded to well rounded. By contrast, the strong angularity of siliciclastic grains in the Gavish Sabkha clearly shows their status as primary weathering products. In all environments studied, insects play a significant role. Mainly salt beetles contribute to the lebensspuren spectrum. There is no indication that burrowing and grazing beetles and dipterans are detrimental to the growing mat systems. According to the marine fauna, two distributional barriers exist: (i) physical and (2) biogeochemical factors. Physical barriers are (a) hypersalinity and barrier-closing, which restrict the marine fauna in the Gavish Sabkha and the Solar Lake to a few species, mainly meiofaunal elements such as ostracods and copepods. Only in the Gavish Sabkha, one marine gastropod species occurs which colonizes mud flats of lower salinity. A salinity barrier of about 70 °/oo separates the gastropod habitats from the zones of growing mats. Under reduced salinity, the snails are able to destroy the microbial mats completely. (b) Decreasing regularity of flooding in the microbial mat environment of Mellum Island excludes intertidal deformative burrowers such as cockles and lugworms. However, locally the mats are pierced by numerous dwelling traces. These stem from small polychaetes and amphipod crustaceans which are able to spread over the intertidal-supratidal boundary and settle up to the MHWS-Ievel. Biogeochemical barriers are oxygen depletion within the sediments, high ammonia and sulfide contents, which generate through bacterial break-down of organic matter. Within the highly productive mats of Mic~ocoleu8 chthonoplastes on Mellum Island, dwelling traces of marine polychaetes and amphipod crustaceans disappear due to these conditions. The name of the mat-forming species, Microcoleus chthonoplastes, indicates its capacity to form "soils" (Greek chthonos). While lithology is not altered, the presence of Mic~ocoleu8 mats leads to a habitat change which excludes trace-making "arenophile" invertebrate species and favors "chthonophile" species which do not leave traces. Stromatolitic microstructures studied in rock specimens were interpreted using modern analogs: Microcolumnar buildups in Precambrian stromatolites, ooids and oncoids were compared with those of modern microbial mats. The nodular to biolaminoid facies type found in the Gavish Sabkha was suggested to be an analog to the Plattendolomite facies of Permian Zechstein, North Poland. Studies of the Lower Jurassic ironstone of Lorraine clearly indicate that fungi have been involved in the formation of stromatolites, ooids and oncoids. In conclusion, the comparative study of microstructures in microbial mats and stromatolites reveals a better understanding in both fields. In many cases, it was geology which first revealed the similarity of recent forms to those ancient ones and consequently encouraged research into them.

Description / Table of Contents: PREFACE It is to-day generally recognized by environmental scientists that the particular behaviour of trace metals in the environment is determined by their specific physico-chemical forms rather than by their total concentration. With the introduction, several years ago, of atomic absorption spectrometry at many laboratories involved in environmental studies, a technique for simple, rapid and cheap determination of total metal concentrations in environmental samples became available. As a consequence, there is a plethora of scientific papers and reports where metal concentrations in the environment are only reported as total concentrations. It appears that the simplicity of making accurate determinations of total metal contents in water, sediment and biological samples has somewhat masked the need for improved knowledge about the various forms of metals occurring in the environment as well as the bioavailahility of these forms. In other words, the need for metal speciation in studies of metals in the environment does not seem to have become obvious to most environmental scientists until relatively recently. As a matter of fact, it was only in the middle of the 1970s that the first systematic attempts were made to obtain information about the various metal species occurring in environmental samples. During the last ten years, however, a revolutionary change of attitude towards the importance of metal speciation has occurred and considerable research effort has been devoted by environmental scientists to measuring the concentrations of biologically important trace metals in surface waters. There is currently an increasing effort to couple the development of chemical analytical techniques to process-related biological problems. Concurrently, a new focus is being imposed on ecological impact studies, that of determining which active trace metal species merit the most intensive research from the standpoint of environmental perturbation. Current efforts are directed towards the development of chemical speciation schemes which can be related directly to measures of bioavailability...

Description / Table of Contents: Early Japanese contributions to space weather research—1945-1960— / A. Nishida / Climate and Weather of the Sun-Earth System (CAWSES): Selected Papers from the 2007 Kyoto Symposium, / pp. 1-22 --- Hydrodynamics, magnetohydrodynamics, and astrophysical plasmas / E. N. Parker / Climate and Weather of the Sun-Earth System (CAWSES): Selected Papers from the 2007 Kyoto Symposium, / pp. 23-40 --- The 1960s—A decade of remarkable advances in middle atmosphere research / M. A. Geller / Climate and Weather of the Sun-Earth System (CAWSES): Selected Papers from the 2007 Kyoto Symposium, / pp. 41-62 --- Hinode "a new solar observatory in space" / S. Tsuneta, L. K. Harra, and S. Masuda / Climate and Weather of the Sun-Earth System (CAWSES): Selected Papers from the 2007 Kyoto Symposium, / pp. 63-75 --- Coronal mass ejections and space weather / N. Gopalswamy / Climate and Weather of the Sun-Earth System (CAWSES): Selected Papers from the 2007 Kyoto Symposium, / pp. 77-120 / © TERRAPUB, Tokyo, 2009. No claim is made to original U.S. Government works. / [Full text] (PDF 3.9 MB) --- Magnetotail after Geotail, Interball and Cluster: Thin current sheets, fine structure, force balance and stability / L. Zelenyi, H. Malova, A. Artemyev, V. Popov, A. Petrukovich, D. Delcourt, and A. Bykov / Climate and Weather of the Sun-Earth System (CAWSES): Selected Papers from the 2007 Kyoto Symposium, / pp. 121-170 --- Simulating solar 'climate' / M. Dikpati / Climate and Weather of the Sun-Earth System (CAWSES): Selected Papers from the 2007 Kyoto Symposium, / pp. 171-199 --- Evidence for solar forcing: Some selected aspects / J. Beer and K. McCracken / Climate and Weather of the Sun-Earth System (CAWSES): Selected Papers from the 2007 Kyoto Symposium, / pp. 201-216 --- Total solar irradiance variability: What have we learned about its variability from the record of the last three solar cycles? / C. Fröhlich / Climate and Weather of the Sun-Earth System (CAWSES): Selected Papers from the 2007 Kyoto Symposium, / pp. 217-230 --- Mechanisms for solar influence on the Earth's climate / J. D. Haigh / Climate and Weather of the Sun-Earth System (CAWSES): Selected Papers from the 2007 Kyoto Symposium, / pp. 231-256 --- Variability in the stratosphere: The sun and the QBO / K. Labitzke and M. Kunze / Climate and Weather of the Sun-Earth System (CAWSES): Selected Papers from the 2007 Kyoto Symposium, / pp. 257-278 --- Gravity wave coupling from below: A review / R. A. Vincent / Climate and Weather of the Sun-Earth System (CAWSES): Selected Papers from the 2007 Kyoto Symposium, / pp. 279-293 --- What we have learnt from CPEA (Coupling Processes in the Equatorial Atmosphere): A review / S. Fukao / Climate and Weather of the Sun-Earth System (CAWSES): Selected Papers from the 2007 Kyoto Symposium, / pp. 295-336 --- Vertical coupling by the semidiurnal tide in Earth's atmosphere / J. M. Forbes / Climate and Weather of the Sun-Earth System (CAWSES): Selected Papers from the 2007 Kyoto Symposium, / pp. 337-348

Description / Table of Contents: Dieses Buch bietet Ihnen umfassendes Excel-Wissen für den beruflichen Alltag. Es ist gleichermaßen Schritt-für-Schritt-Anleitung und Nachschlagewerk sowie eine Fundgrube praktischer Tipps. Lösungsorientiert lernen Sie »on the job« die wichtigsten Funktionen des Programms.

Description / Table of Contents: The Encyclopedia of GIS features an alphabetically arranged comprehensive and authoritative treatment of this subject matter. Authored by world experts and peer-reviewed for accuracy and currency, the entries explain the key software, data sets, and processes used by geographers and computational scientists. Nearly 200 topics include major overviews, such as Geoinformatics, Spatial Cognition, and Location-Based Services. Short entries define specific terms and concepts, such as the Global Positioning System, Digital Elevation/Terrain Model, and Remote Sensing. Larger entries include key citations to the literature, and (online) internal hyperlinks to definitional entries and current standards.The reference will be published as a print volume with abundant black and white art, and simultaneously as an XML online reference with hyperlinked citations, cross-references, four-color art, links to web-based maps, and other interactive features.

Description / Table of Contents: Understanding the process underlying the origin of Earth magnetic field is one of the greatest challenges left to classical Physics. Geomagnetism, being the oldest Earth science, studies the Earth’s magnetic field in its broadest sense. The magnetic record left in rocks is studied in Paleomagnetism. Both fields have applications, pure and applied: in navigation, in the search for minerals and hydrocarbons, in dating rock sequences, and in unraveling past geologic movements such as plate motions they have contributed to a better understanding of the Earth. Consisting of more than 300 articles written by ca 200 leading experts, this authoritative reference encompasses the entire fields of Geomagnetism and Paleomagnetism in a single volume. It describes in fine detail at an assessable level the state of the current knowledge and provides an up-to-date synthesis of the most basic concepts. As such, it will be an indispensable working tool not only for geophysicists and geophysics students but also for geologists, physicists, atmospheric and environmental scientists, and engineers.

Description / Table of Contents: In den ersten zehn Kapiteln des Buches erfahren Sie alles, was Sie zur Shell-Programmierung wissen müssen. Weitere Kapitel gehen auf die unverzichtbaren Tools grep, sed und awk ein, die in Kombination (oder auch allein) mit der Shellscript-Programmierung zu wertvollen Helfern werden können.

Description / Table of Contents: Kaum eine Software, die nicht mehr objektorientiert entworfen und entwickelt wird! Die beiden Autoren geben eine umfassende Einführung in die Prinzipien und die Anwendung der Objektorientierung. Das Buch ist aufgabenorientiert, bietet Beispiele in den Sprachen C++, Java, Ruby, und C# sowie ein Kapitel zur aspektorientierten Programmierung.

Description / Table of Contents: Hier bekommen Sie C-Wissen pur. Egal, ob Sie gerade anfangen, C zu lernen oder ein kompetentes Nachschlagewerk für Fragen rund um C benötigen, mit diesem Buch sind Sie bestens beraten. Ausführlich werden die Grundlagen von C dargestellt, angefangen von den elementaren Datentypen bis hin zu Arrays, Zeigern und dynamischer Speicherverwaltung. Auch fortgeschrittene Themen wie das Programmieren von Webanwendungen mit der CGI-Schnittstelle und eigenen Datenbank-Clients mit der C-API von MySQL, Netzwerk- und Cross-Plattform-Entwicklung kommen nicht zu kurz.

Description / Table of Contents: Wer PHP effizient einsetzen will, sollte die umfangreichen Erweiterungen von PEAR nutzen. Dabei ist PEAR mehr als nur eine einfache Bibliothek. Vergleichbar dem CPAN-Projekt für Perl bietet PEAR zahlreiche Bibliotheken und nützliche Hilfsmittel für PHP-Entwickler, die sich dank des PEAR-Installers auf einfache Weise in bestehende PHP-Installationen integrieren lassen. So lassen sich Entwicklungprozesse erheblich verkürzen. Ein Hindernis stellten bisher lediglich die unzureichnenden Dokumentationen dar. Das Buch von Carsten Möhrke schafft Abhilfe. Es führt in die Nutzung ein, beschreibt ausführlich die Installation und alle wichtigen PEAR- und PECL-Pakete. Auch die Entwicklung eigener Pakete für das Archiv wird beschrieben.

Description / Table of Contents: Dieses Buch bietet einen umfassenden Einblick in die Systemprogrammierung unter Linux und Unix. Es ist für Leser mit Betriebssystem-Kenntnissen und C-Wissen geeignet. Aus dem Inhalt: Umfassende Einführung, E/A-Funktionen, Attribute von Dateien und Verzeichnissen, Zugriff auf Systeminformationen, Prozesse und Dämonprozesse, Umgebungsvariablen eines Prozesses, Signale, Interprozesskommunikation, Threads, Netzwerkprogrammierung, MySQL, Terminal E/A und Benutzerschnittstellen für die Konsole, Sicherheit, XWindow-Programmierung, Windowmanager, Systeminformationen, Devices, GTK+. Neu in dieser 2., erweiterten Auflage: ein Kapitel zu System- und Benutzerdateien, ein stark erweitertes Thread-Kapitel und Ausführungen zu Dämonen, Zombies und Prozessen und zu Unix-Domain-Sockets.

Description / Table of Contents: Dieses Buch bietet Ihnen einen gründlichen und umfassenden Einstieg in die C#-Programmierung. Der erste Teil enthält eine Einführung in .NET, Visual Studio 2008, C# und die objektorientierte Programmierung. Hier werden besonders Einsteiger angesprochen, die noch nicht objektorientiert unter .NET programmiert haben. Im zweiten Teil werden elementare Klassen und Programmiertechniken vorgestellt. Daran schließt sich die Windows-Programmierung an. Großen Raum nimmt die Entwicklung von grafischen Benutzerschnittstellen mit der neuen Windows Presentation Foundation, kurz WPF, ein. Auch ADO.NET und LINQ sind wichtige Themen des Buches.

Description / Table of Contents: Das erste deutsche Rails-Handbuch für Entwickler zur aktuellen Version 2! Hier werden die zahlreichen und komplexen Möglichkeiten des Frameworks ausführlich und verständlich gezeigt. Lesen Sie, wie Sie Rails installieren, wie Sie Ihre ersten Anwendungen erstellen und lernen Sie schließlich alle Module des Frameworks kennen. Das Buch bleibt stets praxisbezogen, da Rails anhand mehrerer »Realworld«-Beispiele erläutert wird. Alle Applikationen sind dabei systematisch aufgebaut, von einfachen bis hin zu komplexen Anwendungen. Für alle, die zum ersten Mal mit Ruby arbeiten, enthält das Buch außerdem eine umfassende Einführung in die Programmiersprache.

Description / Table of Contents: Dieses Buch bietet sowohl eine umfassende Einführung in die Sprache Python als auch viele weiterführende Kapitel zu fortgeschrittenen Themen wie GUI-Entwicklung, Web-Programmierung mit Django oder Netzwerkkommunikation. Nach der Lektüre sind Sie in der Lage, Python professionell einzusetzen. Die Einführung erfolgt systematisch vom ersten einfachen Programm bis hin zu komplexen objektorientierten Programmen. Das Buch ist konsequent praxisorientiert und zum Lernen und Nachschlagen hervorragend geeignet.

Description / Table of Contents: Mechanical properties and fluid transport in rocks are intimately linked as deformation of a solid rock matrix immediately affects the pore space and permeability. The coupling of fluid circulation and deformation processes in crustal rocks results in significant complexity of the mechanical and fluid transport behavior. This often poses severe technical and economic problems for reservoir and geotechnical engineering projects involved in oil and gas production, CO2 sequestration, mining and underground waste disposal. The volume results from the 5th Euroconference on Rock Physics and Geomechanics, which was held in Potsdam, Germany in September 2004. Part I of the topical volume mainly contains contributions investigating the nucleation and evolution of crack damage in rocks, new or modified techniques to measure rock fracture toughness and a discussion of upscaling techniques relating mechanical and fluid transport behavior in rocks at different spatial scales. Part II contains contributions discussing fluid flow and transport in rocks as observed on the laboratory scale and in boreholes. The evolution of rock damage pertinent to the stability of underground excavations is studied and scaling relations of elastic properties and seismic events are discussed.