ALBERT

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 While the complex mechanical properties of rocks and soils are studied for quite a while, it is only in the last decades that sound established mathematical models were developed based on accurate experimental data. Some rheological properties of geomaterials as for instance creep, were studied for a long time but the experimental data reported were incomplete and, as a consequence, the models developed have missed either the generality necessary for the solving of engineering problems or some of the major specific mechanical properties possessed by these materials as for instance dilatancy and/or compressibility , long term damage etc. Generally, these very particular empirical models were made for a specific test only and therefore are not appropriate for solving problems involving general loading histories. Let us remind that due to the presence of a great number of cracks and/or pores existing in roks and soils, the mechanical behaviour of geomaterials is quite distinct from that of other materials as for instance metals or plastics. That is why rock and soil rheology has some specific aspects. It must also be mentioned that the solving of various problems of rock and soil mechanics posed by modern technology was not possible by using time-independent models, thus the study and development of rehological models become absolutely necessary. In the last decade or so, very accurate experimantal data became available as a result of the development of experimental techniques and of the growing interest for this field of research in the scientific community. These data, in turn, have made possible the development of genuine models for geomaterials, mainly rheological models, able to describe such properties as creep, dilatancy and/or compressibility during creep, long term damage and failure occurring after various time intervals, slip surface formation etc. Today it is clear that no accurate constitutive equation for rocks can be formulated unless the dilatancy phenomena and the time effects are not included. Another idea is the need of a better description of the concepts of damage and failure of rocks, again using in someway the concepts of irreversible dilatancy or another related notion. In soil rheology it is clear that the scale effect may be taken into consideration in order to obtain a corect information from the routine tests. Also in writing the constitutive equations for soils it is neccessary to take into account the microscopic or local phenomena, because there is a great variety of types of saturated or nonsaturated soils, granular or cohesionless soil etc. The aim of the Euromech Colloquium 196 devoted to Rock and Soil Rheology and therefore that of the present volume too, is to review some of the main results obtained in the last years in this field of research and also to formulate some of the major not yet solved problems which are now under consideration. Exchange of opinions and scientific discussions are quite helpful mainly in those areas where some approaches are controversial and the progress made is quite fast. That is especially true for the rheology of geomaterials, domain of great interest for mining and petroleum engineers, engineering geology, seismology, geophlsics, civil engineering, nuclear and industrial waste storage, geothermal energy storage, caverns for sports, culture, telecommunications, storage of goods and foodstuffs (cold, hot and refrigerated storages), underground oil and natural gas reservoirs etc. Some of the last obtained results are mentioned in the present volume...

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 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: 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 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: 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 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: 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: 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: Chapter 1: SEDIMENTARY PROCESSES --- Architectural Elements and Bounding Surfaces in Channelized Clastic Deposits: Notes on Comparisons between Fluvial and Turbidite Systems / A. D. MIALL / pp. 3-15 --- A Simulation of Basin Margin Sedimentation to Infer Geometry and Lithofacies—A Carbonate Example— / K. NAKAYAMA and C. G. St. C. KENDALL / pp. 17-31 --- Gravel Fabric of Clast-Supported Resedimented Conglomerate / K. YAGISHITA / pp. 33-42 --- Magnetic Fabrics and Depositional Processes / A. TAIRA / pp. 43-77 --- Chapter 2: FLUVIAL TO COASTAL FACIES --- Sedimentation in Coarse-Grained Sand-Bedded Meanders: Distinctive Deposition of Suspended Sediment / F. ISEYA and H. IKEDA / pp. 81-112 --- Mechanism of Inverse Grading of Suspended Load Deposits / F. ISEYA / pp. 113-129 --- Coastal Eolian Dune Deposits of the Pleistocene Shimosa Group in Chiba, Japan / H. NAKAZATO, H. SATO, and F. MASUDA / pp. 131-141 --- Synsedimentary Conjugate Faults in the Pleistocene Tidal Deposits at Ushibori, Ibaraki, Japan / H. AONO and F. MASUDA / pp. 143-149 --- Description and Genesis of Tidal Bedding in the Cobequid Bay-Salmon River Estuary, Bay of Fundy, Canada / R. W. DALRYMPLE and Y. MAKINO / pp. 151-177 --- Petrofacies of Paleo-Tokyo Bay Sands, the Upper Pleistocene of Central Honshu, Japan / M.ITO and F.MASUDA / pp. 179-196 --- Faunal Condensation in Early Phases of Glacio-Eustatic Sea-Level Rise, Found in the Middle to Late Pleistocene Shimosa Group, Boso Peninsula, Central Japan / Y. KONDO / pp. 197-212 --- Chapter 3: SHALLOW MARINE FACIES --- Sedimentology and History of Sea Level Changes in the East China Sea and Adjacent Seas / B.-C. SUK / pp. 215-231 --- Sediments and Sedimentary Processes in the Yellow and East China Seas / J. D. MILLIMAN, Y. S. QIN, and Y. A. PARK / pp. 233-249 --- Bedforms and Their Migration Patterns in the Southern Bungo Strait, Japan / K. IKEHARA and Y. KIN05HITA / pp. 251-260 --- The Kuroshio-Generated Bedform System in the Osumi Strait, Southern Kyushu, Japan / K. IKEHARA / pp. 261-273 --- Ocean Current-Controlled Sedimentary Facies of the Pleistocene Ichijiku Formation, Kazusa Group, Boso Peninsula, Japan / N. NAKAYAMA and F. MASUDA / pp. 275-293 --- Multi-Layered Progradational Sequences in the Shelf and Shelf Slope of the Southwest Japan Forearc / Y. OKAMURA / pp. 295-318 --- Storm-Built Sand Ridges on the Inner Shelf of Kashima-Nada, Northeast Japan / Y. SAITO / pp. 319-330 --- Storm Deposits in the Inner Shelf and Their Recurrence Intervals, Sendai Bay, Northeast Japan / Modern Y. SAITO / pp. 331-344 --- Sea-Level Controlled Shallow-Marine Systems in the Plio-Pleistocene Kakegawa Group, Shizuoka, Central Honshu, Japan: Comparison of Transgressive and Regressive Phases / M. ISHIBASHI / pp. 345-363 --- Coarse Clastic Sedimentation in the Triassic Offshore Sequence of the South- eastern Kitakami Mountains, Japan / K. KAMADA / pp. 365-375 --- Depositional Facies of the Viséan (Carboniferous) Limestones in the South Kitakami Terrane, Northeast Japan / T. KAWAMURA / pp. 377-391 --- Chapter 4: SLOPE TO DEEP-WATER FACIES --- Depositional Scheme of Neogene Bedded Siliceous Rocks in an Active Upwelling Area-On the Wakkanai Formation, Northern Hokkaido, Japan / H. FUKUSAWA / pp. 395-419 --- Turbidites and Related Clastic Systems in the Tertiary Chichibu Basin, Central Japan / K. M. LATT / pp. 421-438 --- Two Stages of Submarine Fan Sedimentation in an Ancient Forearc Basin, Central Japan / S. TOKUHASHI / pp. 439-468 --- Synsedimentary Folding of a Sandstone Layer: Paleoslope Deduced from the Folding Process / M. FUSEYA / pp. 469-481 --- Miocene Offshore Tractive Current-Worked Conglomerates—Tsubutegaura, Chita Peninsula, Central Japan— / T. YAMAZAKI, M. YAMAOKA, and T. SHIKI / pp. 483-494 --- Coarse Clast Dominant Submarine Debrite, the Mio-Pliocene Fujikawa Group, Central Japan / W. SOH / pp. 495-510 --- Basal Structures of the Pleistocene Chikura Submarine Sliding Sheet in the Southernmost Boso Peninsula, Central Japan / T. ITO and S. SUGIYAMA / pp. 511-528 --- Topography and Sedimentary Facies of the Nankai Deep Sea Channel / K. SHIMAMURA / pp. 529-556 --- Ancient Trench-Fill and Trench-Slope Basin Deposits: An Example from the Permian Nishiki Group, Southwest Japan / A. HARA and K. KIMINAMI / pp. 557-575 --- Tectono-Sedimentary Settings of Seep Biological Communities—A Synthesis from the Japanese Subduction Zones— / K. FUJIOKA and A. TAIRA / pp. 577-602 --- Chapter 5: VOLCANIC FACIES --- Sedimentary Facies of the Mio-Pliocene Volcanotectonic Depressions along the Volcanic Front in Northeast Honshu, Japan / M. UTADA and T. ITO / pp. 605-618 --- Submarine Depositional Processes for Volcaniclastic Sediments in the Mio- Pliocene Misaki Formation, Miura Group, Central Japan / W. SOH, A. TAIRA, Y. OGAWA, H. TANIGUCHI, K. T. PICKERING, and D. A. V. STOW / pp. 619-630 --- Chapter 6: TECTONICS AND SEDIMENTATION --- Upper Cretaceous-Paleogene Kuji Basin of Northeast Japan: Tectonic Controls on Strike-Slip Basin Sedimentation / K. MINOURA and H. YAMAUCHI / pp. 633-658 --- The Itsukaichimachi Group: A Middle Miocene Strike-Slip Basin-Fill in the Southeastern Margin of the Kanto Mountains, Central Honshu, Japan / M. ITO / pp. 659-673 --- Structural Control on Sedimentation of Coal-Bearing Formations in Japan / K. FUJII / pp. 675-688 --- Coarse-Grained Turbidite Sedimentation Resulting from the Miocene Collision Event in Central Hokkaido, Japan / K. HOYANAGI / pp. 689-709 --- Eocene Foreland Thrust-Fold Belt of the Central Ryukyu Island Arc: Deduced from Sedimentary Structures in the Kayo Formation / H. UJIIE / pp. 711-722 --- Rifting of the Gondwanaland and Uplifting of the Himalayas Recorded in Mesozoic and Tertiary Fluvial Sediments in the Nepal Himalayas / H. SAKAI / pp. 723-732

Description / Table of Contents: The problems treated in this volume concern nonlinear partial differential equations occurring in the areas of fluid dynamics, free boundary problems, population dynamics and mathematical physics. Presented are new results and new methods for analysis in bifurcation, singular perturbation, variational methods, stability analysis, rearrangement, energy inequalities, etc

Description / Table of Contents: Ore deposits form by a variety of natural processes that concentrate elements into a volume that can be economically mined. Their type, character and abundance reflect the environment in which they formed and thus they preserve key evidence for the evolution of magmatic and tectonic processes, the state of the atmosphere and hydrosphere, and the evolution of life over geological time. This volume presents 13 papers on topical subjects in ore deposit research viewed in the context of Earth evolution. These diverse, yet interlinked, papers cover topics including: controls on the temporal and spatial distribution of ore deposits; the sources of fluid, gold and other components of orogenic gold deposits; the degree of oxygenation in the Neoproterozoic ocean; bacterial immobilization of gold in the semi-arid near-surface environment; and mineral resources for the future, including issues of resource estimation, sustainability of supply and the criticality of certain elements to society.

Description / Table of Contents: Volcanism and tectonism are the dominant endogenic means by which planetary surfaces change. This book aims to encompass the broad range in character of volcanism, tectonism, faulting and associated interactions observed on planetary bodies across the inner solar system - a region that includes Mercury, Venus, Earth, the Moon, Mars and asteroids. The diversity and breadth of landforms produced by volcanic and tectonic processes is enormous, and varies across the inner solar system bodies. As a result, the selection of prevailing landforms and their underlying formational processes that are described and highlighted in this volume are but a primer to the expansive field of planetary volcanism and tectonism. This Special Publication features 22 research articles about volcanic and tectonic processes manifest across the inner solar system.

Description / Table of Contents: This volume highlights key challenges for fluid-flow prediction in carbonate reservoirs, the approaches currently employed to address these challenges and developments in fundamental science and technology. The papers span methods and case studies that highlight workflows and emerging technologies in the fields of geology, geophysics, petrophysics, reservoir modelling and computer science. Topics include: detailed pore-scale studies that explore fundamental processes and applications of imaging and flow modelling at the pore scale; case studies of diagenetic processes with complementary perspectives from reactive transport modelling; novel methods for rock typing; petrophysical studies that investigate the impact of diagenesis and fault-rock properties on acoustic signatures; mechanical modelling and seismic imaging of faults in carbonate rocks; modelling geological influences on seismic anisotropy; novel approaches to geological modelling; methods to represent key geological details in reservoir simulations and advances in computer visualization, analytics and interactions for geoscience and engineering.

Description / Table of Contents: The discipline of Integrated Environmental Modelling (IEM) has developed in order to solve complex environmental problems, for example understanding the impacts of climate change on the physical environment. IEM provides methods to fuse or link models together, this in turn requires facilities to make models discoverable and also to make the outputs of modelling easily visualized. The vision and challenges for IEM going forward are summarized by leading proponents. Several case studies describe the application of model fusion to a range of real-world problems including integrating groundwater and recharge models within the UK Environment Agency, and the development of ‘catastrophe’ models to predict better the impact of natural hazards. Communicating modelling results to end users who are often not specialist modellers is also an emerging area of research addressed within the volume. Also included are papers that highlight current developments of the technology platforms underpinning model fusion.

Description / Table of Contents: Ernie Rutter has made, and continues to make, a significant impact in the field of rock deformation. He has studied brittle and plastic deformation processes that occur within both the oceanic and continental crust, as well as other key properties such as the permeability and seismic velocities of these rocks. His approach has been one that integrates field observations, laboratory experiments and theoretical analyses. This volume celebrates Ernie's key contribution to rock deformation and structural geology by bringing together a collection of papers that represent this broad approach. The papers within the volume address key issues that remain within these fields. These range from fundamental studies of brittle and plastic behaviour along with the resultant structures and microstructures from both the field and laboratory, to applied problems where a better understanding of the deformation and properties of the crust is still needed.

Description / Table of Contents: Introduction / D. Pereira, B. R. Marker, S. Kramar, B. Cooper and B. Schouenborg / Geological Society, London, Special Publications, 407, 1-4, 23 February 2015, https://doi.org/10.1144/SP407.18 --- Procedures and criteria for the definition of Global Heritage Stone Resources / Brian R. Marker / Geological Society, London, Special Publications, 407, 5-10, 10 June 2014, https://doi.org/10.1144/SP407.3 --- The ‘Global Heritage Stone Resource’ designation: past, present and future / Barry J. Cooper / Geological Society, London, Special Publications, 407, 11-20, 21 May 2014, https://doi.org/10.1144/SP407.5 --- Global stone heritage: Larvikite, Norway / Tom Heldal, G. B. Meyer and R. Dahl / Geological Society, London, Special Publications, 407, 21-34, 27 November 2014, https://doi.org/10.1144/SP407.14 --- The Hallandia gneiss, a Swedish heritage stone resource / B. Schouenborg, J. Andersson, M. Göransson and Inger Lundqvist / Geological Society, London, Special Publications, 407, 35-48, 4 November 2014, https://doi.org/10.1144/SP407.17 --- The Kolmården serpentine marble in Sweden: a stone found both in castles and people's homes / Anders Wikström and Dolores Pereira / Geological Society, London, Special Publications, 407, 49-56, 28 January 2015, https://doi.org/10.1144/SP407.22 --- Global Heritage Stone: Estremoz Marbles, Portugal / Luís Lopes and Ruben Martins / Geological Society, London, Special Publications, 407, 57-74, 15 August 2014, https://doi.org/10.1144/SP407.10 --- Contribution of Portuguese two-mica granites to stone built heritage: the historical value of Oporto granite / Angela Almeida and Arlindo Begonha / Geological Society, London, Special Publications, 407, 75-91, 27 November 2014, https://doi.org/10.1144/SP407.16 --- Piedra Pajarilla: a candidacy as a global heritage stone resource for Martinamor granite / Dolores Pereira, Ana Gimeno and Santiago Del Barrio / Geological Society, London, Special Publications, 407, 93-100, 21 May 2014, https://doi.org/10.1144/SP407.6 --- The Sierra Nevada serpentinites: the serpentinites most used in Spanish heritage buildings / Rafael Navarro, Dolores Pereira, Carlos Rodríguez-Navarro and Eduardo Sebastián-Pardo / Geological Society, London, Special Publications, 407, 101-108, 10 June 2014, https://doi.org/10.1144/SP407.7 --- Villamayor Stone (Golden Stone) as a Global Heritage Stone Resource from Salamanca (NW of Spain) / J. Garcia-Talegón, A. C. Iñigo, G. Alonso-Gavilán and S. Vicente-Tavera / Geological Society, London, Special Publications, 407, 109-120, 27 November 2014, https://doi.org/10.1144/SP407.19 --- Colmenar Limestone, Madrid, Spain: considerations for its nomination as a Global Heritage Stone Resource due to its long term durability / R. Fort, M. J. Varas-Muriel, M. Alvarez de Buergo and E. M. Perez-Monserrat / Geological Society, London, Special Publications, 407, 121-135, 3 September 2014, https://doi.org/10.1144/SP407.8 --- Carrara Marble: a nomination for ‘Global Heritage Stone Resource’ from Italy / P. Primavori / Geological Society, London, Special Publications, 407, 137-154, 23 February 2015, https://doi.org/10.1144/SP407.21 --- Rosa Beta granite (Sardinian Pink Granite): a heritage stone of international significance from Italy / N. Careddu and S. Grillo / Geological Society, London, Special Publications, 407, 155-172, 21 May 2014, https://doi.org/10.1144/SP407.1 --- Pietra Serena: the stone of the Renaissance / F. Fratini, E. Pecchioni, E. Cantisani, S. Rescic and S. Vettori / Geological Society, London, Special Publications, 407, 173-186, 3 September 2014, https://doi.org/10.1144/SP407.11 --- Ornamental stones of the Verbano Cusio Ossola quarry district: characterization of materials, quarrying techniques and history and relevance to local and national heritage / Giovanna A. Dino and Alessandro Cavallo / Geological Society, London, Special Publications, 407, 187-200, 15 October 2014, https://doi.org/10.1144/SP407.15 --- Stone materials used for monumental buildings in the historical centre of Turin (NW Italy): architectonical survey and petrographic characterization of Via Roma / Alessandro Borghi, Valentina Berra, Anna d'Atri, Giovanna A. Dino, Lorenzo M. Gallo, Elena Giacobino, Luca Martire, Gianluca Massaro, Gloria Vaggelli, Carlo Bertok, Daniele Castelli, Emanuele Costa, Simona Ferrando, Chiara Groppo and Franco Rolfo / Geological Society, London, Special Publications, 407, 201-218, 27 November 2014, https://doi.org/10.1144/SP407.20 --- Podpeč limestone: a heritage stone from Slovenia / S. Kramar, M. Bedjanič, B. Mirtič, A. Mladenović, B. Rožič, D. Skaberne, M. Gutman, N. Zupančič and B. Cooper / Geological Society, London, Special Publications, 407, 219-231, 10 June 2014, https://doi.org/10.1144/SP407.2 --- Stone heritage in Southeast Slovenia / M. Golež and B. Mirtič / Geological Society, London, Special Publications, 407, 233-242, 27 August 2014, https://doi.org/10.1144/SP407.12 --- Ornamental stone in the history of St Petersburg architecture / A. G. Bulakh / Geological Society, London, Special Publications, 407, 243-252, 10 June 2014, https://doi.org/10.1144/SP407.4 --- Natural stone in the built heritage of the interior of Brazil: the use of stone in Minas Gerais / A. G. Costa / Geological Society, London, Special Publications, 407, 253-261, 22 July 2014, https://doi.org/10.1144/SP407.13 --- ‘Piedra Mar del Plata’: An Argentine orthoquartzite worthy of being considered as a ‘Global Heritage Stone Resource’ / F. Cravero, M. B. Ponce, M. R. Gozalvez and S. A. Marfil / Geological Society, London, Special Publications, 407, 263-268, 8 July 2014, https://doi.org/10.1144/SP407.9

Description / Table of Contents: Introduction --- Selection of Plants that Demonstrated Nitrate Removal Characteristics --- Inspection and Maintenance Guidelines

Description / Table of Contents: Three centuries (1670–1970) of appreciating physical landscapes / Thomas A. Hose / Geological Society, London, Special Publications, 417, 1-23, 11 September 2015, https://doi.org/10.1144/SP417.15 --- Appreciating geology and the physical landscape in Scotland: from tourism of awe to experiential re-engagement / John E. Gordon and Matt Baker / Geological Society, London, Special Publications, 417, 25-40, 12 January 2015, https://doi.org/10.1144/SP417.1 --- Waterfalls and the Romantic traveller / Brian J. Hudson / Geological Society, London, Special Publications, 417, 41-57, 12 January 2015, https://doi.org/10.1144/SP417.9 --- The artist as geotourist: Eugene von Guérard and the seminal sites of early volcanic research in Europe and Australia / Ruth Pullin / Geological Society, London, Special Publications, 417, 59-69, 15 December 2014, https://doi.org/10.1144/SP417.4 --- Landscape and geotourism on the Dutch coast in the seventeenth century as depicted by landscape artists / J. A. M. (Hanneke) van den Ancker and Pieter Dirk Jungerius / Geological Society, London, Special Publications, 417, 71-82, 14 October 2015, https://doi.org/10.1144/SP417.14 --- Visitors to ‘the northern playgrounds’: tourists and exploratory science in north Norway / W. Brian Whalley and Anne F. Parkinson / Geological Society, London, Special Publications, 417, 83-93, 17 September 2015, https://doi.org/10.1144/SP417.12 --- The role of local societies in early modern geotourism: a case study of the Chester Society of Natural Science and the Woolhope Naturalists’ Field Club / Cynthia V. Burek and Thomas A. Hose / Geological Society, London, Special Publications, 417, 95-116, 6 February 2015, https://doi.org/10.1144/SP417.6 --- Geotourism: an early photographic insight through the lens of the Geologists’ Association / Jonathan G. Larwood / Geological Society, London, Special Publications, 417, 117-129, 18 December 2014, https://doi.org/10.1144/SP417.7 --- The contribution of maps to appreciating physical landscape: examples from Derbyshire's Peak District / C. John Henry and Thomas A. Hose / Geological Society, London, Special Publications, 417, 131-155, 7 September 2015, https://doi.org/10.1144/SP417.13 --- Three centuries of open access to the caves in Stoney Middleton Dale Site of Special Scientific Interest, Derbyshire / Mark A. Cope / Geological Society, London, Special Publications, 417, 157-169, 30 October 2014, https://doi.org/10.1144/SP417.3 --- Geology and landscape in SW England in the late eighteenth century, as recorded in the travel journals of William George Maton (1774–1840) / John D. Mather / Geological Society, London, Special Publications, 417, 171-185, 13 November 2014, https://doi.org/10.1144/SP417.8 --- The role of Carclaze tin mine in eighteenth and nineteenth century geotourism / Colin Bristow / Geological Society, London, Special Publications, 417, 187-197, 11 February 2015, https://doi.org/10.1144/SP417.11 --- From tourism to geotourism: a few historical cases from the French Alpine foreland / Nathalie Cayla, Christophe Gauchon and Fabien Hobléa / Geological Society, London, Special Publications, 417, 199-213, 11 February 2015, https://doi.org/10.1144/SP417.10 --- Rediscovering geoheritage, reinventing geotourism: 200 years of experience from the Sudetes, Central Europe / Piotr Migoń / Geological Society, London, Special Publications, 417, 215-228, 13 November 2014, https://doi.org/10.1144/SP417.2 --- Appreciating loess landscapes through history: the basis of modern loess geotourism in the Vojvodina region of North Serbia / Djordjije A. Vasiljević, Slobodan B. Marković and Miroslav D. Vujičić / Geological Society, London, Special Publications, 417, 229-239, 3 November 2014, https://doi.org/10.1144/SP417.5

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