ALBERT

Description / Table of Contents: Imaging, mapping and modelling continental lithosphere extension and breakup: an introduction, G D Karner, G Manatschal and L M Pinheiro. - Break-up of the Newfoundland-Iberia rift, B E Tucholke, D S Sawyer and J-C Sibuet. - Structure of the Flemish Cap margin, Newfoundland: insights into mantle and crustal processes during continental breakup, J R Hopper, T Funck and B E Tucholke. - Early Cretaceous motion of Flemish Cap with respect to North America: implications on the formation of Orphan Basin and SE Flemish Cap-Galicia Bank conjugate margins, J-C Sibuet, S P Srivastava, M Enachescu and G D Karner. - The formation of non-volcanic rifted margins by the progressive extension of the lithosphere: the example of the West Iberian margin, T J Reston. - Roles of lithospheric strain softening and heterogeneity in determining the geometry of rifts and continental margins, R S Huismans and C Beaumont. - The role of gravitational instabilities, density structure, and extension rate in the evolution of continental margins, E Burov. - A dynamic model of rifting between Galicia Bank and Flemish Cap during opening of the North Atlantic Ocean, D L Harry and S Grandell. - A kinematic modelling approach to lithosphere deformation and basin formation: application to the Black Sea, S S Egan and D J Meredith. - Early kinematic history of the Goban Spur rifted margin derived from a new model of continental breakup and sea-floor spreading initiation, D Healy and N J Kusznir. - The boundary between continental rifting and seafloor spreading in the Woodlark Basin, Papua New Guinea, A M Goodliffe and B Taylor. - Nature of the continent-ocean transition zone along the southern Australian continental margin: a comparison of the Naturaliste Plateau, SW Australia, and the central Great Australian Bight sectors, N G Direen, I Borissova, H M J Stagg, J B Colwell and P A Symonds. - Constraints on the deformation and rupturing of continental lithosphere of the Red Sea: the transition from rifting to drifting, J R Cochran and G D Karner. - Observations from the Alpine Tethys and Iberia Newfoundland margins pertinent to the interpretation of continental breakup, G Manatschal, O Muntener, L L Lavier, T A Minshull and G Peron-Pinvidic. - Overview of tectonic settings related to the rifting and opening of Mesozoic ocean basins in the Eastern Tethys: Oman, Himalayas and Eastern Mediterranean regions, A H F Robertson. - Continental lithospheric thinning and breakup in response to upwelling divergent mantle flow: application to the Woodlark, Newfoundland, and Iberia margins, N J Kusznir G D Karner. - Observations from the Basin and Range Province (western United States) pertinent to the interpretation of regional detachment faults, N Christie-Blick, M H Anders, S Wills, C D Walker and B Renik. - Effects of initial weakness on rift architecture, S Dyksterhuis, P Rey, R D Müller and L Moresi. - Incompressible viscous formulations for deformation and yielding of the lithosphere, L Moresi, H-B Muhlhaus, V Lemiale and D May.

Description / Table of Contents: This book summarizes our present understanding of the formation of passive continental margins and their ocean–continent transitions. It outlines the geological, geophysical and petrological observations that characterize extensional systems, and how such observations can guide and constrain dynamic and kinematic models of continental lithosphere extension, breakup and the inception of organized sea-floor spreading. The book focuses on imaging, mapping and modelling lithospheric extensional systems, at both the regional scale using dynamic models to the local scale of individual basins using kinematic models, with an emphasis on capturing the extensional history of the Iberia and Newfoundland margins. The results from a number of other extensional regimes are presented to provide comparisons with the North Atlantic studies; these range from the Tethyan realm and the northern Red Sea to the western and southern Australian margins, the Basin and Range Province, and the Woodlark basin of Papua New Guinea. All of these field studies, combined with lessons learnt from the modelling, are used to address fundamental questions about the extreme deformation of continental lithosphere.

Description / Table of Contents: The Devonian was a peculiar period, characterized by simplified plate tectonic configurations, climatic overheating and widely flooded continents. The bloom of fishes and ammonoids, extensive reef complexes, and the conquest of land indicate major biosphere innovations, punctuated by many global events, including two of the biggest mass extinctions. The Devonian was the first system for which subdivisions were formally defined. This was achieved by significant advances in pelagic biostratigraphy. The chronostratigraphic framework and interdisciplinary techniques allow us to correlate intervals or sudden events across facies boundaries, in order to reconstruct the sedimentary and evolutionary history of the system with highest precision. This volume honors the lifetime stratigraphic achievements of Michael Robert House (1930-2002). Based on case studies from Europe, North Africa and North America, it shows how the combination of biostratigraphy, chemostratigraphy, magnetostratigraphy, sequence stratigraphy and event stratigraphy can contribute to a much deeper understanding of both regional and global environmental change.

Description / Table of Contents: We are poised to embark on a new era of discovery in the study of geomorphology. The discipline has a long and illustrious history, but in recent years an entirely new way of studying landscapes and seascapes has been developed. It involves the use of 3D seismic data. Just as CAT scans allow medical staff to view our anatomy in 3D, seismic data now allows Earth scientists to do what the early geomorphologists could only dream of - view tens and hundreds of square kilometres of the Earth's subsurface in 3D and therefore see for the first time how landscapes have evolved through time. This volume demonstrates how earth scientists are starting to use this relatively new tool to study the dynamic of a range of sedimentary environments.

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: For the geoscientist, interest in sediment dynamics relates to the understanding of modern processes, together with their extrapolation to the interpretation of ancient deposits within the stratigraphic record. Over the years, various measurement techniques and scientific approaches have been applied to the determination of sediment transport pathways and the derivation of erosion, transport and deposition rates. Recently, a number of new techniques and approaches have been developed, associated with different temporal and spatial scales, and it is appropriate and timely to review a representative selection, by reference to recently undertaken coastal and shelf investigations. The various contributions in the volume cover, for example: optical and acoustic backscatter measurements; particle tracking; the use of mutibeam imagery; grain-size trend analysis; and analytic, numerical and conceptual modelling. Although no single method provides a complete solution to the problem posed, this overview will assist sedimentologists and sediment dynamicists in their selection of the most appropriate approaches, towards the establishment of ‘high confidence’ in the interpretation of sediment transport rates and directions.

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: Structurally complex reservoirs form a distinct class of reservoir in which fault arrays and fracture networks, in particular, exert an overriding control on petroleum trapping and production behaviour. With modern exploration and production portfolios now commonly held in geologically complex settings, there is an increasing technical challenge to find new prospects and to extract remaining hydrocarbons from these reservoirs. This volume reviews our current understanding and ability to model the complex distribution and behaviour of fault and fracture networks, highlighting their fluid compartmentalizing effects and storage-transmissivity characteristics, and outlining approaches for predicting the dynamic fluid flow and geomechanical behaviour of these reservoirs. This collection of 25 papers provides an overview of recent progress and outstanding issues in the areas of (i) structural complexity and fault geometry, (ii) detection and prediction of faults and fractures, (iii) compartmentalizing effects of fault systems and complex siliciclastic reservoirs and (iv) critical controls affecting fractured reservoirs.

Description / Table of Contents: The complexity of plate interactions and associated crustal deformation in the Eastern Mediterranean region is reflected by the numerous destructive earthquakes that have occurred throughout its history. Many of these have been well documented and studied. In addition, the Aegean region provides examples of core-complex formation, synchronous basin evolution and subsequent graben formation and continental extensional deformation following orogenic contraction. It is therefore considered to be a perfect natural laboratory for the study of these mechanisms. The region has been the subject of intensive research for several decades. This book contains current results and ideas regarding the geodynamics of the Aegean and Anatolia. It will be essential reading for all geoscientists with an interest in the structural evolution of the Eastern Mediterranean.

Description / Table of Contents: In the last four centuries geologists have traversed the globe, searching for economically important materials or simply to satisfy their intellectual curiosity. Geologists have often been at the vanguard of scientific exploration. The microscopist Robert Hooke explored the Isle of Wight, and Charles Darwin the Cape Verde islands and parts of South America. The volcanic wonders of Italy and central France attracted native and foreign visitors including Lyell and Murchison. The Tyrrell brothers faced great hardship in northern Canada, as did the actor and mineralogist Charles Lewis Giesecke in Greenland. The development of Sydney, Australia depended on finding limestone for building. French geologists relied on camels in the Sahara, and Grenville Cole trusted his tricycle to carry him across Europe. Four Centuries of Geological Travel: The Search for Knowledge on Foot, Bicycle, Sledge and Camel focuses on the complexities of geological exploration and will be of particular interest to Earth scientists, historians of science and to the general reader interested in science.

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: This book is an exploration of varying approaches to the study of the deposition, diagenesis and stratigraphy of evaporites. The volume includes papers from chemical modellers, who work on the basis of geochemical representations of the formative water bodies, and from basin-wide depositional-stratigraphical modellers, who propose depositional scenarios that are fitted to individual basinal pictures. Until now there have been only a few studies of evaporite formation that explain the characteristic features we observe in the real rock record. This volume is a collection of relevant papers in which these features are integrated in a realistic manner, based on our new understanding of saline water bodies, to the diverse tectonic, chemical and depositional constraints of their individual basins. In additional there are several review articles that offer oversight and extensive referencing of basins worthy of further study. This book is a valuable resource for sedimentologists and stratigraphers looking for an up-to-date reference on evaporite deposits.

Description / Table of Contents: The North China craton is the only known place where an Archaean craton with a thick tectospheric root lost half of that root in younger tectonism by processes such as delamination, convection, hydration-weakening, compositional change or some other mechanism. In this volume, authors provide data constraining the geometry and timing of root loss, aimed at understanding why and how continental roots are lost in general. Modelling how often this process may have occurred in the geological past, and how much lithospheric material has been recycled to the convecting mantle through this mechanism, could drastically change our current understanding of crustal growth rates and processes. Possible triggering mechanisms for root loss include collision of the South China (Yangtze) and North China cratons in the Triassic, the India–Asia collision, closure of the Solonker and Monhgol–Okhotsk oceans, Mesozoic subduction of the Pacific Plate beneath eastern China, impingement of mantle plumes, mantle hydration from long-term subduction and several rifting events. In this volume, we link studies of crustal tectonics with investigations aimed at determining the nature of and timing of the formation and loss of the root, in order to better-understand mechanisms of continental root formation, evolution and recycling/removal.

Description / Table of Contents: The geological record contains a fascinating diversity of reefs and shell accumulations. As my other biosedimentary structures, their facies characterization requires careful observation at outcrop and sample scale, and in thin-section to provide information about the global geometries, fabrics and textures respectively. This collection of papers encompasses the breadth of sedimentary geometries and facies displayed by Palaeozoic reefs, shell accumulations, and transitional composite deposits. The definition of reefs and shell concentrations has given rise to variations in nomenclature. The papers in this volume cover specific problems regarding the nomenclature and facies characterization of reefs, shell accumulations and transitional composite deposits. However, rather than attempt a complete revision of terms, the authors have touched on some of the important issues at this stage of development in the field: the main climatic, environmental and evolutionary factors that controlled the Palaeozoic development of shell accumulation and reefs.

Description / Table of Contents: This book is the first peer-reviewed collection of papers focusing on the potential of myth storylines to yield data and lessons that are of value to the geological sciences. Building on the nascent discipline of geomythology, scientists and scholars from a variety of disciplines have contributed to this volume. The geological hazards (such as earthquakes, tsunamis, volcanic eruptions and cosmic impacts) that have given rise to myths are considered, as are the sacred and cultural values associated with rocks, fossils, geological formations and landscapes. There are also discussions about the historical and literary perspectives of geomythology. Regional coverage includes Europe and the Mediterranean, Afghanistan, Cameroon, India, Australia, Japan, Pacific islands, South America and North America. Myth and Geology challenges the widespread notion that myths are fictitious or otherwise lacking in value for the physical sciences.

Description / Table of Contents: Stone buildings and monuments from the cultural centres of many of the world's urban areas. Frequently these areas are prone to high levels of atmospheric pollution that promote a variety of aggressive stone decay processes. Because of this, stone decay is now widely recognized as a severe threat to much of our cultural heritage. If this threat is to be successfully addressed it is essential that the symptoms of decay are clearly identified, that appropriate stone properties are accurately characterized and that decay processes are precisely identified. It is undoubtedly the case that successful conservation has to be underpinned by a comprehensive understanding of the causes of decay and the factors that control them. The accomplishment of these demanding goals requires an interdisciplinary approach based on co-operation between geologists, environmental scientists, chemists, material scientists, civil engineers, restorers and architects. In pursuit of this collaboration, this volume aims to strengthen the knowledge base dealing with the causes, consequences, prevention and solution of stone decay problems.

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: 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 dangers that we face from geohazards appear to be getting worse, especially with the impact of increasing population and global climate change. This collection of papers illustrates how remote sensing technologies - measuring, mapping and monitoring the Earth's surface from aircraft or satellites - can help us to rapidly detect and better manage geohazards. The hazardous terrains examined include areas of landslides, flooding, erosion, contaminated land, shrink-swell clays, subsidence, seismic activity and volcanic landforms. Key aspects of remote sensing are introduced, making this a book that can easily be read by those who are unfamiliar with remote sensing. The featured remote sensing systems include aerial photography and photogrammetry, thermal scanning, hyperspectral sensors, airborne laser altimetry (LiDAR), radar interferometry and multispectral satellites (Landsat, ASTER). Related technologies and methodogies, such as the processing of Digital Elevation Models and data analysis using Geographical Information Systems, are also discussed.

Description / Table of Contents: Where were the women in Geology? This book is a first as it unravels the diverse roles women have played in the history and development of geology as a science predominantly in the UK, Ireland and Australia, and selectively in Germany, Russia and US. The volume covers the period from the late eighteenth century to the present day and shows how the roles that women have played changed with time. These included illustrators, museum collectors and curators, educationalists, researchers and geologists. Originally as wives, sisters or mothers many were assistants to their male relatives. This book looks at all these forgotten women and for the first time historians and scientists together explore the contribution they made to this male-dominated subject. There are individual profiles on remarkable women: Catherine Raisin, Dorothea Bate, Cuvier's daughters, Grace Prestwich, Annie Greenly, Nancy Kirk, Margaret Crosfield, Ethel Skeat, Maria Ogivlie Gordon, Marie Stopes, Anne Phillips, Muriel Arber and Etheldred Bennett. Pulling together this extensive research uncovered common issues and generated emergent themes. The Editors have brought this new research together under these themes and tried to answer the question Where were the women in Geology? They go on to discuss how these role models can be applicable to today's society.

Description / Table of Contents: Fractured reservoirs contain a significant proportion of the global hydrocarbon reserves; however, they commonly exhibit unpredictable and extreme production behaviour. To develop such reservoirs it is necessary to obtain the best understanding possible of the fracture network and its impact on the fluid flow within the reservoir, using the full range of geoscience and engineering datasets available at all scales. This book presents an overview of current techniques and the latest technologies used to understand and exploit fractured reservoirs. The contributions are organized into sections on outcrop analogues, the application of geophysical techniques for fracture detection and imaging, numerical and analogue modelling and case studies from fields in the Middle East, Europe and North America. A number of the case studies also consider ways of assessing uncertainties in fracture geometry description and the implications for effective reservoir management.

Description / Table of Contents: The many kinds of porous geomaterials (rocks, soils, concrete, etc.) exhibit a range of responses when undergoing inelastic deformation. In doing so they commonly develop well-ordered fabric elements, forming fractures, shear bands and compaction bands, so creating the planar fabrics that are regarded as localization. Because these induced localization fabrics alter the bulk material properties (such as permeability, acoustic characteristics and strength), it is important to understand how and why localization occurs, and how it relates to its setting. The concept of damage (in several uses) describes both the precursor to localization and the context within which it occurs. A key theme is that geomaterials display a strong material evolution during deformation, revealing a close linkage between the damage and localization processes. This volume assembles perspectives from a number of disciplines, including soil mechanics, rock mechanics, structural geology, seismic anisotropy and reservoir engineering. The papers range from theoretical to observational, and include contributions showing how the deformed geomaterials emergent bulk characteristics, like permeability and seismic anisotropy, can be predicted. This book will be of interest to a wide range of geoscientists and engineers who deal with characterization of deformed materials.

Description / Table of Contents: The study of reservoir and repository performance requires the integration of many different fields in Earth sciences, among them rock physics and geomechanics. The aim of this book is to emphasize how rock physics and geomechanics help to get a better insight into important issues linked to reservoir management for exploitation of natural resources, and to repository safety assessment for hazardous waste storage in geological environment. The studies presented here deal with the hydromechanical coupling in fractured rocks, the key experiments in safety assessment of repositories, the development of damaged zones during excavation in a shaley formation, the influence of temperature on the properties of shales, the poroelastic response of sandstones, the development and propagation of compaction bands in reservoir rocks, imaging techniques of geomaterials, the characterization and modelling of reservoirs using 4D seismic data, the mechanical behaviour of fractured rock masses, the petrophysical properties of fault zones, models for rock deformation by pressure solution and the elastic anisotropy in cracked rocks.

Description / Table of Contents: The Eastern Mediterranean region is a classic area for the study of tectonic processes and settings related to the development of the Tethyan orogenic belt. The present set of research and synthesis papers by Earth scientists from countries in this region and others provides an up-to-date, interdisciplinary overview of the tectonic development of the Eastern Mediterranean region from Precambrian to Recent. Key topics include continental rifting, ophiolite genesis and emplacement, continental collision, extensional tectonics, crustal exhumation and intra-plate deformation (e.g. active faulting). Alternative tectonic reconstructions of the Tethyan orogen are presented and discussed, with important implications for other regions of the world. The book will be an essential source of information and interpretation for academic researchers (geologists and geophysicists), advanced undergraduates and also for industry professionals, including those concerned with hydrocarbons, minerals and geological hazards (e.g. earthquakes).

Description / Table of Contents: Earth sciences are becoming ever more concerned with how their disciplines, their research and teaching, need to become directly related to environmental and social concerns. The biology of the surface layers and at depth is increasingly important in the geosciences. A knowledge of biological and physical-chemical functions in terrestrial ecosystems (such as biomass production, filtering, buffering and transformation, water routing, and maintenance of biodiversity) that are studied in soil science provides a background for Earth sciences. The papers in this volume address issues of soil formation, soil management, soil protection and the role of biodiversity that must be considered for a sustainable soil use. The papers are aimed at geoscientists in the broadest sense, and others concerned with soil use who will also find chapters relevant to their interests. Soils knowledge used within other Earth sciences is essential for maintaining healthy ecosystems, for the solutions of problems in environmental quality and for sustainable use of soils by humans.

Description / Table of Contents: Contents: New techniques in sediment core analysis: an introduction, R G Rothwell and F R Rack .- The Eagle III BKA system, a novel sediment core X-ray fluorescence analyser with very high spatial resolution, M Haschke. - The AVAATECH XRF Core Scanner: technical description and applications to NE Atlantic sediments, T O Richter, S Van Der Gaast, R Koster, A Vaars, R Gieles, H C de Stigter, H de Haas and T C E van Weering . - ITRAX: description and evaluation of a new multi-function X-ray core scanner, I W Croudace, A Rindby and R G Rothwell. - A geochemical application of the ITRAX scanner to a sediment core containing eastern Mediterranean sapropel units, J Thomson, I W Croudace and R G Rothwell . - Turbidite emplacement on the southern Balearic Abyssal Plain (western Mediterranean Sea) during Marine Isotope Stages 1-3: an application of ITRAX XRF scanning of sediment cores to lithostratigraphic analysis, R G Rothwell, B Hoogakker, J Thomson, I W Croudace and M Frenz. - Colour logging as a tool in high-resolution palaeoceanography, M Rogerson, P P E Weaver, E J Rohling, L J Lourens, J W Murray and A Hayes . - Sediment colour analysis from digital images and correlation with sediment composition, A J Nederbragt, R B Dunbar, A T Osborn, A Palmer, J W Thurow and T Wagner . - Sediment mineralogy based on visible and near-infrared reflectance spectroscopy, R D Jarrard and M D Vanden Berg . - Applications of confocal macroscope microscope luminescence imaging to sediment cores, A C Ribes, F R Rack, G Tsintzouras, S Damaskinos and A E Dixon . - Pressure coring, logging and sub-sampling with the HYACINTH system, P J Schultheiss, T J G Francis, M Holland, J A Roberts, H Amann, Thjunjoto, R J Parkes, D Martin, M Rothfuss, F Tyunder, and P D Jackson . - On-site geological core analysis using a portable X-ray computed tomographic system, B M Freifeld, T J Kneafsey and F R Rack . - Nuclear magnetic resonance pore-scale investigation of permafrost and gas hydrate sediments, R L Kleinberg . - Quantitative magnetic resonance imaging methods for core analysis, Q Chen, F R Rack and B J Balcom . - Rapid non-contacting resistivity logging of core, P D Jackson, M A Lovell, J A Roberts, P J Schultheiss, D Gunn, R C Flint, A Wood, R Holmes and T Frederichs . - Logging-while-coring - new technology from the simultaneous recovery of downhole cores and geophysical measurements, D Goldberg, G Myers, G J Iturrino, K Grigar, T Pettigrew and S Mrozewski . - Integration of the stratigraphic aspects of the very large sea-floor databases using information processing, C Jenkins, J Flocks and M Kulp . - Core data stewardship: a long-term perspective, C J Moore and R E Habermann. - The Janus database: providing worldwide access to ODP and IODP data, R Mithal and D G Becker.

Description / Table of Contents: Die Frage ist nicht, ob fossile Energieträger (insbesondere das Erdöl) endlich sind, sondern wie bald die Quellen endgültig versiegen. 3 Jahre nach seinem beachtlichen Debüt "Öko-Realismus" (BA 2/03), das Gründinger (geboren 1984) als Oberstufenschüler vorgelegt hatte, beschäftigt sich der Student der Politikwissenschaften und Mitglied von Youth for Intergenerational Justice und Sustainability - Europe (YOIS) eingehend mit der brisanten Energiefrage. Die "pyromane" Menschheit verbrenne sich selbst, sei durch die Abhängigkeit von der "schwarzen Droge Öl" in eine bedrohliche Falle geraten, aus der sie sich kaum befreien könne. Sein Abgesang auf die fossil-atomare Energieversorgung, die kritische Analyse des gegenwärtigen Energiesystems und sein propagierter "Weg in ein Industrielles Solarzeitalter" (Energie-Revolution) speisen sich aus einem breiten Fundus an aktuellen Daten und Fakten aus Fachliteratur, aber auch geheimgehaltenen Dokumenten. Mit Bibliografie. Wie H. Scheer: "Energieautonomie" (BA 10/05) ein wichtiger, kompetenter Beitrag zum Thema, diesmal der jüngeren Generation. Sehr empfohlen. (2) (Helga Lüdtke)

Description / Table of Contents: Abgesang auf die fossil-atomare Energieversorgung, kritische Analyse des gegenwärtigen Energiesystems und propagierter "Weg in ein Industrielles Solarzeitalter" (Energie-Revolution) eines Umweltaktivisten der jüngeren Generation. (Helga Lüdtke)

Description / Table of Contents: Gullies on Mars resemble terrestrial gullies involved in the transport of abundant material down steep slopes by liquid water. However, liquid water should not be stable at the Martian surface. The articles in this volume present the two main opposing theories for Martian gully formation: climate-driven melting of surficial water-ice deposits and seasonal dry-ice sublimation. The evidence presented ranges from remote-sensing observations, to experimental simulations, to comparison with Earth analogues. The opposing hypotheses imply either that Mars has been unusually wet in the last few million years or that it has remained a cold dry desert – both with profound implications for understanding the water budget of Mars and its habitability. The debate questions the limits of remote-sensing data and how we interpret active processes on extra-terrestrial planetary surfaces, even beyond those on Mars, as summarized by the review paper at the beginning of the book.

Description / Table of Contents: Contents: Vorwort ; Einführung: Was heißt Kyoto Plus? ; 1 Die Welt sitzt in der Treibhausfalle: Sie steuert Richtung Klimakatastrophe ; 2 Die katastrophalen Auswirkungen des Klimawandels ; 3 Das bestehende "Kyoto 1"-Klimaschutzsystem- äußerst wichtig aber nahezu unwirksam ; 4 "Mikrotropfen auf den heißen Klimastein" - eine klimapolitisch gefährliche Strategie ; 5 Kyoto Plus: Die Mindestvoraussetzungen für ein wirksames System ; 6 Kyoto Plus: Seine beispielhafte Umsetzung durch das globale Klimazertifikatsystem als konkret entwickeltes Cap-and-Trade-System ; 7 Kyoto-Plus: Welweiter Durchbruch klimafreundlicher Produktions- und Konummuster zur Sicherstellung des Klimazieles ; 8 KyotoPlus: Weltweit nachhaltige statt klimabedrohende Energieversorgung- und nutzung durch das globale Cap-and Trade-System ; 9 Entwicklungs- und Schwellenländer: Ohne Gerechtigkeit keine Klimarettung ; 10 Finanzierung und Durchsetzung der Ökosozialen Marshallpläne zur nachhaltigen, klimafreundlichen Entwicklung und Armutsbeseitigung ; 11 Kyoto Plus: Die beste "angemessene Maßnahme" zur "Verhinderung gefährlicher Störungen des Klimasystems" ; 12 Die Widerstände der Industrieländer gegen Kyoto Plus sind überwindbar ; 13 Die Entwicklungsländer: Pro Kyoto Plus ; 14 Klimaallianzen pro wirksamen Klimaschutz: Der Erfolg versprechende Weg zur Durchsetzung von Kyoto Plus ; 15 Klimarettung als moralische Pflicht ; 16 Zehn gute Argumente für die internationale Durchsetzbarkeit von Kyoto Plus ; Literaturverzeichnis

Description / Table of Contents: This book complements the Geological Society's Special Publication 362: Military Aspects of Hydrogeology. Generated under the auspices of the Society's History of Geology and Engineering Groups, it contains papers from authors in the UK, USA, Germany and Austria. Substantial papers describe some innovative engineering activities, influenced by geology, undertaken by the armed forces of the opposing nations in World War I. These activities were reactivated and developed in World War II. Examples include trenching from World War I, tunnelling and quarrying from both wars, and the use of geologists to aid German coastal fortification and Allied aerial photographic interpretation in World War II. The extensive introduction and other chapters reveal that ‘military geology’ has a longer history. These chapters relate to pre-twentieth century coastal fortification in the UK and the USA; conflict in the American Civil War; long-term ‘going’ assessments for German forces; tunnel repair after wartime route denial in Hong Kong; and tunnel detection after recent insurgent improvisation in Iraq.

Description / Table of Contents: Contents: 1 Vom Wetter zum Klima ; 2 Es werde Luft ; 3 Klima und Leben ; 4 Klima und Evolution im Erdaltertum ; 5 Klima und Evolution im Erdmittelalter ; 6 Vom Treibhaus zum Eishaus ; 7 Klima und die Evolution der Primaten ; 8 Klima und Evolution im Pliozan ; 9 Klima und die Evolution des Menschen im Eiszeitalter ; 10. Klima und Mensch im Holozän ; 11 Klimaentwicklung seit der Industriellen Revolution ; 12 Klimawandel und Klimaschutz ; 13 Klimaforschung und Klimaprognosen ; 14 Die Zukunft des Planeten Erde ; Erde, Klima, Leben - Ein Nachwort

Description / Table of Contents: Analogue and numerical sandbox model. - Models of orogenic processes. - Models of sedimentary basins. - Models of surface processes and deformation. - Models of faults and fluid flow .

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: 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: This Special Publication has 24 papers with an international authorship, and is prefaced by an introductory overview which presents highlights in the field. The first section covers the acceptance by science of the reality of the falls of rock and metal from the sky, an account that takes the reader from BCE (before common era) to the nineteenth century. The second section details some of the world's most important collections in museums - their origins and development. The Smithsonian chapter also covers the astonishingly numerous finds in the cold desert of Antarctica by American search parties. There are also contributions covering the finds by Japanese parties in the Yamato mountains and the equally remarkable discoveries in the hot deserts of Australia, North Africa, Oman and the USA. The other seven chapters take the reader through the revolution in scientific research on meteoritics in the later part of the twentieth century, including terrestrial impact cratering and extraordinary showers of glass from the sky; tektites, now known to be Earth-impact-sourced. Finally, the short epilogue looks to the future. The History of Meteoritics and Key Meteorite Collections should appeal to historians of science, meteoriticists, geologists, astronomers, curators and the general reader with an interest in science.

Description / Table of Contents: The seismically and volcanically active East African Rift System is an ideal laboratory for continental break-up processes: it encompasses all stages of rift development. Its northernmost sectors within the Afar volcanic province include failed rifts, nascent seafloor spreading, and youthful passive continental margins associated with one or more mantle plumes. A number of models have been proposed to explain the success and failure of continental rift zones, but there remains no consensus on how strain localizes to achieve rupture of 125–250 km thick plates, or on the interaction between the plates and asthenospheric processes. This collection of papers provides new structural, stratigraphic, geochemical and geophysical data and numerical models needed to resolve fundamental questions concerning continental break-up and mantle plume processes. It focuses on how mantle melt intrudes and is distributed through the plate, and how this magma intrusion process controls along-axis segmentation and facilitates break-up.

Description / Table of Contents: This volume gives a broad view of the application of geoscience techniques to the study of monuments and objects from excavations and museums, including their origin, technique of manufacture, age and conservation. It reaffirms the important contribution of geosciences in the interdisciplinary approach to the study of complex materials such as minerals, rocks, glass, metals, mortar, plaster, slags and pottery. The papers in this book cover three topics: the study of pottery, glass, stone and mortar; the application of Raman spectroscopy to a wide variety of objects; and the future of archaeometry. Interdisciplinary studies including field geology, geophysics, microscopy, textural analysis, physical methods and geochemistry are used to unlock information from the ancient materials, such as the provenance of the raw materials, the firing technology, the ancient recipes, and the alteration pathways.

Description / Table of Contents: During the past decade, work on cool water carbonates has expanded to become a mainstream research area. Studies on modern and Quaternary deposits will continue to be important; however, there is increasing momentum towards unravelling sediment processes, biota-sediment interactions and diagenetic products in Cenozoic and older cool-water carbonates. Many contributions in this book document Cenozoic and Quaternary carbonates from landlocked (microtidal) water-bodies. These carbonates display important differences in biota and fabric distributions when compared with world ocean examples. Consequently, the scientific community is now better placed to reinterpret pre-Tertiary carbonates where there is a suspicion that they have developed under microtidal conditions. Some papers in the book provide new approaches to interpreting environmental change within macrotidal regimes and others lay firm foundations for future cool-water carbonate diagenetic research. The aim of the book is to illustrate recent international contributions to cool-water carbonates research, with an emphasis on Neogene and Recent case studies. Contributions are divided into three sections: microtidal carbonates from the Mediterranean realm; macrotidal examples from New Zealand, Australia and Mexico; and early diagenetic fabrics.

Description / Table of Contents: Large caldera collapses represent catastrophic natural events, second only to large meteoritic impacts. In addition, some calderas are densely populated, making the risk extreme, even for moderate eruptions. Understanding caldera mechanisms, unrest and the danger of eruption is therefore a crucial challenge for Earth sciences. Several key features of caldera behaviour have yet to be fully understood. Through a combination of case studies and theoretical modelling, the following topics are addressed in this volume: the conditions required to produce and to release large volumes of magma erupted during caldera formation; how magmatic feeding systems evolve before and after a caldera has formed; the processes that limit the behaviour of precursors to eruptions; how pre-emptive precursors can be distinguished from those that drive unrest without an eruption; and given that post-collapse eruptions may occur across a wide area, the optimum procedures for designing hazard maps and mitigation strategies.

Description / Table of Contents: Marine sediment cores are the fundamental data source for information on seabed character, depositional history and environmental change. They provide raw data for a wide range of research including studies of climate change, palaeoceanography, slope stability, oil exploration, pollution assessment and control, seafloor survey for laying cables, pipelines and construction of seafloor structures. During the last three decades, a varied suite of new technologies have been developed to analyse cores, often non-destructively, to produce high-quality, closely spaced, co-located downcore measurements. These techniques can characterize sediment physical properties, geochemistry and composition in unprecedented detail. Palaeoenvironmentally significant proxies can now be logged at decadal, and in some cases, annual or sub-annual scales, allowing highly detailed insights into climatic history and associated environmental change. These advances have had a profound effect on many aspects of the Earth Sciences and our understanding of the Earth's history. In this volume, recent advances in analytical and logging technology and their application to the analysis of sediment cores are presented. Developments in providing access to core data and associated datasets, and advances in data mining technology in order to integrate and interpret new and legacy datasets within the wider context of seafloor studies are also discussed.

Description / Table of Contents: Earth sciences are becoming ever more concerned with how their disciplines, their research and teaching, need to become directly related to environmental and social concerns. The biology of the surface layers and at depth is increasingly important in the geosciences. A knowledge of biological and physical-chemical functions in terrestrial ecosystems (such as biomass production, filtering, buffering and transformation, water routing, and maintenance of biodiversity) that are studied in soil science provides a background for Earth sciences. The papers in this volume address issues of soil formation, soil management, soil protection and the role of biodiversity that must be considered for a sustainable soil use. The papers are aimed at geoscientists in the broadest sense, and others concerned with soil use who will also find chapters relevant to their interests. Soils knowledge used within other Earth sciences is essential for maintaining healthy ecosystems, for the solutions of problems in environmental quality and for sustainable use of soils by humans.

Description / Table of Contents: During the Permian, the single supercontinent Pangaea stretched from pole to pole. Early Permian glacial deposits are found in southern Gondwana. Along the sutures of Pangaea, mountain ranges towered over vast tropical lowlands. Interior areas included dry deserts where dune sands accumulated. Gypsum and halite beds document the evaporation of hot, shallow seas that formed the most extensive salt deposits in the geological record. The Permian period (251 to 299 Ma) encompasses nine ages (stages) arranged into three epochs (series). Most of the Permian marine timescale has been defined by global stratotype sections and points for the stage boundaries. This volume presents new data regarding the biostratigraphy and biochronology of the non-marine Permian and provides a basis for temporally ordering Permian geological and biotic history on land, and correlating that history to events in the marine realm.

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: This book provides an insight into the overall tectonic evolution of the Western Mediterranean region and North Africa. The tectonic setting of the region reflects a long-lived and complex evolution, mainly related to the Alpine Orogeny. This inheritance is expressed by an intricate pattern of arc-shaped mountain chains, the Alps, the Betic-Rif Cordilleras and the Apennine-Maghrebian belt, whose southern branches mark the present limit between the African and Eurasian plates. The volume covers the Maghrebian chains in North Africa, from Tunisia to Morocco and the Western and Central Mediterranean, from Spain to Italy from the pre-orogeric phases (Palaeozoic-Mesozoic) to the post-collisional neotectonic and Quaternary development. It includes both original research papers and syntheses dealing with the aspects of structural, sedimentary, metamorphic and marine geology.

Description / Table of Contents: Analogue and Numerical Sandbox Models --- Analogue benchmarks of shortening and extension experiments / Guido Schreurs, Susanne J. H. Buiter, David Boutelier, Giacomo Corti, Elisabetta Costa, Alexander R. Cruden, Jean-Marc Daniel, Silvan Hoth, Hemin A. Koyi, Nina Kukowski, Jo Lohrmann, Antonio Ravaglia, Roy W. Schlische, Martha Oliver Withjack, Yasuhiro Yamada, Cristian Cavozzi, Chiara Del Ventisette, Jennifer A. Elder Brady, Arne Hoffmann-Rothe, Jean-Marie Mengus, Domenico Montanari and Faramarz Nilforoushan / Geological Society, London, Special Publications, 253, 1-27, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.01 --- The numerical sandbox: comparison of model results for a shortening and an extension experiment / Susanne J. H. Buiter, Andrey Yu. Babeyko, Susan Ellis, Taras V. Gerya, Boris J. P. Kaus, Antje Kellner, Guido Schreurs and Yasuhiro Yamada / Geological Society, London, Special Publications, 253, 29-64, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.02 --- Models of Orogenic Processes --- Interaction between normal faults and pre-existing thrust systems in analogue models / Giacomo Corti, Serena Lucia, Marco Bonini, Federico Sani and Francesco Mazzarini / Geological Society, London, Special Publications, 253, 65-78, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.03 --- Surface topography and internal strain variation in wide hot orogens from three-dimensional analogue and two-dimensional numerical vice models / Alexander R. Cruden, Mohammad H. B. Nasseri and Russell Pysklywec / Geological Society, London, Special Publications, 253, 79-104, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.04 --- Relative importance of trenchward upper plate motion and friction along the plate interface for the topographic evolution of subduction-related mountain belts / Andrea Hampel and Adrian Pfiffner / Geological Society, London, Special Publications, 253, 105-115, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.05 --- Deformation transfer in viscous detachments: comparison of sandbox models to the South Pyrenean Triangle Zone / Hemin A. Koyi and Maura Sans / Geological Society, London, Special Publications, 253, 117-134, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.06 --- Analogue modelling of a reactivated, basement controlled strike-slip zone, Sierra de Albarracín, Spain: application of sandbox modelling to polyphase deformation / S. Merten, W. G. Smit, D. A. Nieuwland and H. E. Rondeel / Geological Society, London, Special Publications, 253, 135-152, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.07 --- Lithospheric scale gravitational flow: the impact of body forces on orogenic processes from Archaean to Phanerozoic / Patrice F. Rey and Gregory Houseman / Geological Society, London, Special Publications, 253, 153-167, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.08 --- Analogue and numerical modelling of accretionary prisms with a décollement in sediments / Yasuhiro Yamada, Kei Baba and Toshifumi Matsuoka / Geological Society, London, Special Publications, 253, 169-183, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.09 --- Models of Sedimentary Basins --- Integrated four-dimensional modelling of sedimentary basin architecture and hydrocarbon migration / S. M. Clarke, S. D. Burley, G. D. Williams, A. J. Richards, D. J. Meredith and S. S. Egan / Geological Society, London, Special Publications, 253, 185-211, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.10 --- Rifting through a heterogeneous crust: insights from analogue models and application to the Gulf of Corinth / L. Mattioni, L. Le Pourhiet and I. Moretti / Geological Society, London, Special Publications, 253, 213-231, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.11 --- 3D modelling of rifting through a pre-existing stack of nappes in the Gulf of Corinth (Greece): a mixed analogue/numerical approach / L. Le Pourhiet, L. Mattioni and I. Moretti / Geological Society, London, Special Publications, 253, 233-252, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.12 --- Inversion of a symmetric basin: insights from a comparison between analogue and numerical experiments / M. Panien, S. J. H. Buiter, G. Schreurs and O. A. Pfiffner / Geological Society, London, Special Publications, 253, 253-270, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.13 --- Lower crustal rheological expression in inverted basins / Mike Sandiford, David L. Hansen and Sandra N. McLaren / Geological Society, London, Special Publications, 253, 271-283, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.14 --- Geometric and experimental models of extensional fault-bend folds / Martha O. Withjack and Roy W. Schlische / Geological Society, London, Special Publications, 253, 285-305, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.15 --- Models of Surface Processes and Deformation --- Recent advances and current problems in modelling surface processes and their interaction with crustal deformation / Jean Braun / Geological Society, London, Special Publications, 253, 307-325, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.16 --- Macroscale dynamics of experimental landscapes / Stephane Bonnet and Alain Crave / Geological Society, London, Special Publications, 253, 327-339, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.17 --- Numerical modelling of erosion processes in the Himalayas of Nepal: effects of spatial variations of rock strength and precipitation / V. Godard, J. Lavé and R. Cattin / Geological Society, London, Special Publications, 253, 341-358, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.18 --- Models of Faults and Fluid Flow --- Effects of compaction processes on stresses, faults, and fluid flow in sedimentary basins: examples from the Norwegian margin / Knut Bjørlykke / Geological Society, London, Special Publications, 253, 359-379, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.19 --- Multiple faults in ductile simple shear: analogue models of flanking structure systems / Ulrike Exner, Bernhard Grasemann and Neil S. Mancktelow / Geological Society, London, Special Publications, 253, 381-395, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.20 --- Using an elastic dislocation model to investigate static Coulomb stress change scenarios for earthquake ruptures in the eastern Marmara Sea region, Turkey / Jordan R. Muller, Atilla Aydin and Tim J. Wright / Geological Society, London, Special Publications, 253, 397-414, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.21 --- Oil reservoirs in foreland basins charged by thrustbelt source rocks: insights from numerical stress modelling and geometric balancing in the West Carpathians / Michal Nemčok and Andreas Henk / Geological Society, London, Special Publications, 253, 415-428, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.22 --- Relation between effective friction and fault slip rate across the Northern San Andreas fault system / Ann-Sophie Provost and Jean Chéry / Geological Society, London, Special Publications, 253, 429-436, 1 January 2006, https://doi.org/10.1144/GSL.SP.2006.253.01.23

Description / Table of Contents: Sandstone aquifers are common worldwide: they contain a significant proportion of the Earth’s fresh water supplies. However, because of their textural complexity and the frequent occurrence of both matrix and fracture flow, prediction of flow and pollutant migration is still a considerable challenge. This volume contains a collection of papers summarizing current research on an example sandstone aquifer: the UK Permo-Triassic Sandstone sequence. These red bed, organic-poor sandstones are of fluvial and aeolian origin, are often strongly textured, and are cut by discontinuities of a wide range of permeabilities. Matrix flow often dominates, but fracture flow also occurs. The papers in the volume deal with research on saturated and unsaturated flow, and solute and non-aqueous-phase liquid movement. They cover investigations from laboratory to regional scale, and involve a wide range of approaches, from petrophysical through geophysical and hydrochemical to modelling. The book is intended to be of interest to researchers and practitioners involved in water resources and groundwater pollution, and to hydrogeology, water engineering, and environmental science students.

Description / Table of Contents: In the Earth sciences, the concept of fractals and scale invariance is well recognized in many natural objects. However, the use of fractals for spatial and temporal analyses of natural hazards has been less used (and accepted) in the Earth sciences. This book brings together 12 contributions that emphasize the role of fractal analyses in natural hazard research, including andslides, wildfires, floods, catastrophic rock fractures and earthquakes. A wide variety of spatial and temporal fractal-related approaches and techniques are applied to ‘natural’ data, experimental data and computer simulations. These approaches include probabilistic hazard analysis, cellular-automata models, spatial analyses, temporal variability, prediction and self-organizing behaviour. The main aims of this volume are (a) to present current research on fractal analyses as applied to natural hazards and (b) to stimulate the curiosity of advanced Earth science students and researchers in the use of fractals analyses for the better understanding of natural hazards.

Description / Table of Contents: The Eastern Mediterranean region is a classic area for the study of tectonic processes and settings related to the development of the Tethyan orogenic belt. The present set of research and synthesis papers by Earth scientist from countries in this region and others provides an up-to-date, interdisciplinary overview of the tectonic development of the Eastern Mediterrenean region from Precambrian to Recent. Key topics include continental rifting, ophiolite genesis and emplacement, continental collision, extensional tectonics, crustal exhumation and intraplate deformation (e.g. active faulting). Alternative tectonic reconstructions of the Tethyan orogen are presented and discussed, with important implications for other regions of the world. The book will be an essential source of information and interpretation for academic researchers (geologists and geophysicists), advanced undergraduates and also for industry professionals, including those concerned with hydrocarbons, minerals and geological hazards (e.g. earthquakes).

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.