ALBERT

Description / Table of Contents: Preface / John Mather / Geological Society, London, Special Publications, 225, vi, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.01 --- 200 years of British hydrogeology — an introduction and overview / J. D. Mather / Geological Society, London, Special Publications, 225, 1-13, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.02 --- The water-related work of William Smith (1769–1839) / H. S. Torrens / Geological Society, London, Special Publications, 225, 15-30, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.03 --- Dr John Snow and an early investigation of groundwater contamination / Michael Price / Geological Society, London, Special Publications, 225, 31-49, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.04 --- William Whitaker (1836–1925) — geologist, bibliographer and a pioneer of British hydrogeology / William H. George / Geological Society, London, Special Publications, 225, 51-65, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.05 --- Joseph Lucas (1846–1926) — Victorian polymath and a key figure in the development of British hydrogeology / J. D. Mather, H. S. Torrens and K. J. Lucas / Geological Society, London, Special Publications, 225, 67-88, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.06 --- 19th century studies of the hydrogeology of the Permo-Triassic Sandstones of the northern Cheshire Basin, England / John H. Tellam / Geological Society, London, Special Publications, 225, 89-105, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.07 --- Robert Stephenson (1803–1859) — the first groundwater engineer / M. Preene / Geological Society, London, Special Publications, 225, 107-119, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.08 --- ‘Making water’: the hydrogeological adventures of Britain’s early mining engineers / Paul L. Younger / Geological Society, London, Special Publications, 225, 121-157, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.09 --- The contribution of geologists to the development of emergency groundwater supplies by the British army / Edward P. F. Rose / Geological Society, London, Special Publications, 225, 159-182, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.10 --- Groundwater versus surface water in Scotland and Ireland — the formative years / N. S. Robins, J. R. P. Bennett and K. T. Cullen / Geological Society, London, Special Publications, 225, 183-191, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.11 --- Bath thermal waters: 400 years in the history of geochemistry and hydrogeology / W. Mike Edmunds / Geological Society, London, Special Publications, 225, 193-199, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.12 --- Chalybeate springs at Tunbridge Wells: site of a 17th-century new town / J. G. C. M. Fuller / Geological Society, London, Special Publications, 225, 201-212, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.13 --- The Scottish hydropathic establishments and their use of groundwater / Iain Spence and Nick Robins / Geological Society, London, Special Publications, 225, 213-217, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.14 --- British hydrogeologists in North Africa and the Middle East: an historical perspective / J. W. Lloyd / Geological Society, London, Special Publications, 225, 219-227, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.15 --- British hydrogeologists in West Africa — an historical evaluation of their role and contribution / Robin Hazell / Geological Society, London, Special Publications, 225, 229-237, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.16 --- British attempts to develop groundwater and water supply on Gibraltar 1800–1985 / Edward P.F. Rose, John D. Mather and Manuel Perez / Geological Society, London, Special Publications, 225, 239-262, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.17 --- The first use of geophysics in borehole siting in hardrock areas of Africa / Ron Barker / Geological Society, London, Special Publications, 225, 263-269, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.18 --- The development of groundwater in the UK between 1935 and 1965 — the role of the Geological Survey of Great Britain / R. A. Downing / Geological Society, London, Special Publications, 225, 271-282, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.19 --- Jack Ineson (1917–1970) The instigator of quantitative hydrogeology in Britain / R. A. Downing and D. A. Gray / Geological Society, London, Special Publications, 225, 283-286, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.20 --- Stevenson Buchan (1907–1996): field geologist, hydrogeologist and administrator / D. A. Gray and J. D. Mather / Geological Society, London, Special Publications, 225, 287-293, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.21 --- Groundwater studies in the Institute of Geological Sciences between 1965 and 1977 / D. A. Gray / Geological Society, London, Special Publications, 225, 295-318, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.22 --- Norman Savage Boulton (1899–1984): civil engineer and groundwater hydrologist / R. A. Downing, W. Eastwood and K. R. Rushton / Geological Society, London, Special Publications, 225, 319-322, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.23 --- Groundwater in a national water strategy, 1964–1979 / R. A. Downing / Geological Society, London, Special Publications, 225, 323-338, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.24 --- Recollections of a golden age: the groundwater schemes of Southern Water 1970–1990 / H. G. Headworth / Geological Society, London, Special Publications, 225, 339-362, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.25 --- Developments in UK hydrogeology since 1974 / F. C. Brassington / Geological Society, London, Special Publications, 225, 363-385, 1 January 2004, https://doi.org/10.1144/GSL.SP.2004.225.01.26

Description / Table of Contents: The wide distribution of dolomite rocks in North American, Middle- and Far-Eastern hydrocarbon reservoirs is reason enough for their intensive study. In this volume dolomite enthusiasts review progress and define the current boundaries of dolomite research, related particularly to the importance of these rocks as reservoirs. As might be expected, reviews provide critical analyses of past ideas on origins and why many are no longer tenable. Discussions range between conceptual models and numerical simulations of the flow paths of dolomitizing fluids, geochemical modelling, and microbial mediation. Case studies from areas as diverse as North America, the Middle East, SE Asia and Australia provide a solid background but illustrate important differences in views on the origins of these enigmatic rocks.

Description / Table of Contents: This book gives an up-to-date overview of the physical geology of sub-volcanic intrusions. Topics covered in this wide-ranging volume include important aspects of the field geology and physical volcanology of sills, laccoliths and sub-volcanic complexes, magma-sediment interaction and numerical and experimental studies aimed at quantifying more precisely the emplacement mechanics of high-level magmatic intrusions. Provocative papers ask whether laccoliths and high-level sills are forming today, and question the nature of the relationship between high-level intrusions and contemporaneous volcanic activity. Several contributions also deal with the more applied aspects of high-level magma emplacement and 3D seismic imaging of sill and laccolith complexes as relevant to the hydrocarbons industry. It is hoped that with the publication of this volume a consensus will emerge that will help to advance our understanding of the more important physical factors governing the emplacement of high-level intrusions in the continental crust, along with their wider geotectonic implications.

Description / Table of Contents: The Cretaceous submarine Ontong Java Plateau, in the western Pacific Ocean, is the most volumnous of the world's large igneous provinces(LIPs), and represents the largest known magmatic event on Earth. LIPs are the products of basaltic volcanism on a scale and at an effusion rate not seen on Earth at the present time, and their formation may have had significant effects on the Earth's climate and biosphere. The currently favoured explanation for LIP formation is the rapid decompression and melting of anomalously hot mantle in the heads of newly ascended mantle plumes. This volume summarizes the results of research aimed principally at testing the plume-head hypothesis for the formation of the Ontong Java Plateau, and presents the results of integrated studies following recent basement drilling on the plateau by the Ocean Drilling Program Nineteen papers cover topics as diverse as petrology, geochemistry, tectonics, volcanology, paleomagnatism and biostratigraphy.

Description / Table of Contents: Bivalves are key components of Recent marine and freshwater ecosystems and have been so for most of the Phanerozoic. Their rich and long fossil record, combined with their abundance and diversity in modern seas, has made bivalves the ideal subject of palaeobiological and evolutionary studies. Despite this, however, topics such as the early evolution of the class, relationships between various taxa and the life habits of some key extinct forms have remained remarkably unclear. In the last few years there has been enormous expansion in the range of techniques available to both palaeontologists and zoologists and key discoveries of new faunas which shed new light on the evolutionary biology of this important class. This volume integrates palaeontological and zoological approaches and sheds new light on the course of bivalve evolution. This series of 32 original papers tackles key issues including: up to date molecular phylogenies of major groups; new hard and soft tissue morphological cladistic analyses; reassessments of the early Palaeozoic radiation; important new observations on form and functional morphology; analyses of biogeography and biodiversity; novel (palaeo)ecological studies

Description / Table of Contents: Concepts and Models --- The falling stage systems tract: recognition and importance in sequence stratigraphic analysis / A. Guy Plint and Dag Nummedal / Geological Society, London, Special Publications, 172, 1-17, 1 January 2000, https://doi.org/10.1144/GSL.SP.2000.172.01.01 --- Aspects of the stratal architecture of forced regressive deposits / Henry W. Posamentier and William R. Morris / Geological Society, London, Special Publications, 172, 19-46, 1 January 2000, https://doi.org/10.1144/GSL.SP.2000.172.01.02 --- Palaeozoic-Mesozoic --- Carbonate megabreccias in a sequence stratigraphic context; evidence from the Cambrian of North Greenland / Jon R. Ineson and Finn Surlyk / Geological Society, London, Special Publications, 172, 47-68, 1 January 2000, https://doi.org/10.1144/GSL.SP.2000.172.01.03 --- Shingled, sharp-based shoreface sandstones: depositional response to stepwise forced regression in a shallow basin, Upper Triassic Gassum Formation, Denmark / Lars Hamberg and Lars Henrik Nielsen / Geological Society, London, Special Publications, 172, 69-89, 1 January 2000, https://doi.org/10.1144/GSL.SP.2000.172.01.04 --- The significance of the Etive Formation in the development of the Brent system: distinction of normal and forced regressions / Tina R. Olsen and Ron J. Steel / Geological Society, London, Special Publications, 172, 91-112, 1 January 2000, https://doi.org/10.1144/GSL.SP.2000.172.01.05 --- Forced regressions: recognition, architecture and genesis in the Campanian of the Bighorn Basin, Wyoming / Roy Fitzsimmons and Steve Johnson / Geological Society, London, Special Publications, 172, 113-139, 1 January 2000, https://doi.org/10.1144/GSL.SP.2000.172.01.06 --- Style contrast between forced regressive and lowstand/transgressive wedges in the Campanian of south-central Wyoming (Hatfield Member of the Haystack Mountains Formation) / Donatella Mellere and Ronald Steel / Geological Society, London, Special Publications, 172, 141-162, 1 January 2000, https://doi.org/10.1144/GSL.SP.2000.172.01.07 --- Forward stratigraphic modelling of forced regressions: evidence for the genesis of attached and detached lowstand systems / R. B. Ainsworth, H. Bosscher and M. J. Newall / Geological Society, London, Special Publications, 172, 163-176, 1 January 2000, https://doi.org/10.1144/GSL.SP.2000.172.01.08 --- Cenozoic --- Tectonically enhanced forced regressions: examples from growth folds in extensional and compressional settings, the Miocene of the Suez rift and the Eocene of the Pyrenees / Robert L. Gawthorpe, Matt Hall, Ian Sharp and Tom Dreyer / Geological Society, London, Special Publications, 172, 177-191, 1 January 2000, https://doi.org/10.1144/GSL.SP.2000.172.01.09 --- Recognition and distinction of normal and forced regression in cyclothemic strata: a Plio-Pleistocene case study from eastern North Island, New Zealand / Douglas W. Haywick / Geological Society, London, Special Publications, 172, 193-215, 1 January 2000, https://doi.org/10.1144/GSL.SP.2000.172.01.10 --- Response of Plio-Pleistocene mixed bioclastic-lithoclastic temperate-water carbonate systems to forced regressions: the Calcarenite di Gravina Formation, Puglia, SE Italy / Marcello Tropeano and Luisa Sabato / Geological Society, London, Special Publications, 172, 217-243, 1 January 2000, https://doi.org/10.1144/GSL.SP.2000.172.01.11 --- Quaternary forced regression deposits in the Adriatic basin and the record of composite sea-level cycles / Fabio Trincardi and Annamaria Correggiari / Geological Society, London, Special Publications, 172, 245-269, 1 January 2000, https://doi.org/10.1144/GSL.SP.2000.172.01.12 --- Depositional response to Quaternary fourth-order sea-level fluctuations on the Latium margin (Tyrrhenian Sea, Italy) / Francesco L. Chiocci / Geological Society, London, Special Publications, 172, 271-289, 1 January 2000, https://doi.org/10.1144/GSL.SP.2000.172.01.13 --- Sequence stratigraphy and architecture of the Late Pleistocene Lagniappe delta complex, northeast Gulf of Mexico / V. Kolla, P. Biondi, B. Long and R. Fillon / Geological Society, London, Special Publications, 172, 291-327, 1 January 2000, https://doi.org/10.1144/GSL.SP.2000.172.01.14 --- Seismic stratigraphy of the Gulf of Cádiz continental shelf: a model for Late Quaternary very high-resolution sequence stratigraphy and response to sea-level fall / F. J. Hernández-Molina, L. Somoza and F. Lobo / Geological Society, London, Special Publications, 172, 329-362, 1 January 2000, https://doi.org/10.1144/GSL.SP.2000.172.01.15 --- Along-strike variability of forced regressive deposits: late Quaternary, northern Peloponnesos, Greece / Lesley S. McMurray and Robert L. Gawthorpe / Geological Society, London, Special Publications, 172, 363-377, 1 January 2000, https://doi.org/10.1144/GSL.SP.2000.172.01.16

Description / Table of Contents: The flow of glacier ice can produce structures that are striking and beautiful. Associated sediments,too, can develop spectacular deformation structures, and examples are remarkbly well preserved in Quaternary deposits. Although such features have long been recognized, they are now the subject of new attention from glaciologists and glacial geologists. This collection of papers addresses how the methods for unravelling deformation structures evolved in recent years by structural geologists can be used for glacial materials, and the opportunities offered to structural geologists by glacial materials for studying deformation in rocks.

Description / Table of Contents: The ten articles in this book describe the mode of emplacement of various types of intrusions (salt diapirs, mud volcanoes and magmatic bodies) by means of theoretical reasoning, analogue and analytical modelling, interpretation of seismic and field data, and geodetic surveying. All the articles emphasize the role of regional tectonics in driving or controlling the emplacement of the intrusions. The selection of articles includes examples from Spain, Romania, onshore and offshore Italy, the Eastern Mediterranean, Israel and iran. Better understanding of the mode of emplacement of these intrusions has applications in hydrocarbon exploration (e.g., where salt structures or mud diapirs are present) and in the mining industry (where mineralization is related to the emplacement of batholiths).

Description / Table of Contents: This volume contains 23 papers from a range of international contributors, describing recent research into the tectonics and magmatism of Turkey and its surroundings. This region is sited at the collision zone between Eurasia and Afro-Arabia and, as such, provides an extraordinarily complete and well-exposed record of the staged tectonic evolution of this sector of the Alpine-Himalayan orogen. The geological history of this area involves separation of continental fragments from the margin of Gondwana, their migration across the Tethyan oceans, the subsequent closure of these oceans and, finally, the development of the neotectonic regime, which continues to evolve to the present day. Such a comprehensive record is relevant to the understanding of collisional zones worldwide. The volume is divided into five sections: Tethyan evolution, Neotethyan ophiolites, post-Tethyan basin evolution, neotectonics and igneous activity. The first two sections deal with Tethyan oceans, whose growth and subsequent closure dominated the geodynamic framework in the Mesozoic and Cenozoic. The subsequent sections deal with more recent geological developments from the Balkan Peninsula in the west to the Transcaucasus in the east that followed consumption of the Tethyan oceans. There is a broad mix of papers throughout the volume: wide-ranging review papers on ocean development and extensional tectonics are followed by detailed descriptions of petrology and geochemistry and geographically focused studies on basin evolution, specific aspects of extensional and strike-slip tectonics and discussions of the relationship of magmatic activity to the tectonic development of the area.

Description / Table of Contents: Geological prior information represents a new and emerging field within the geosciences. Prior information is the term used to describe previously existing knowledge that can be brought to bear on a new problem. This volume describes a range of methods that can be used to find solutions to practical and theoretical problems using geological prior information, and the nature of geological information that can be so employed. As such, this volume defines how geology can be influential far beyond the confines of its own definition.

Description / Table of Contents: This publication reflects a growing appreciation of yhe extent to which turbidite depositional system development is fundamentally affected by basin-floor topography. In the many turbidite and turbidite hydrocarbon reservoirs, depositional patterns have been moderately to strongly confined by pre-existing slopes; thus 'submarine fans' may be far from fan-shaped where constrained by significant bathymetric features. This volume examines aspects of sediment dispersal and accumulation in deep-water systems where sea-floor topography has exerted a decisive control on deposition, and explores the associated controls on hydrocarbon reservoir architecture and heterogeneity. The papers presented here offer a global perspective, which is wide-ranging in terms of approach as well as location, including contrasting reviews and case studies of outcrop, subsurface, modern and experimental systems. This book will be of use both to academic geologists and to geoscience professionals in industry dealing with characterization and modelling of deep-water clastic reservoirs.

Description / Table of Contents: Recycling of oceanic plate back into the Earth’s interior at subduction zones is one of the key processes in Earth evolution. Volcanic arcs, which form above subduction zones, are the most visible manifestations of plate tectonics, the convection mechanism by which the Earth loses excess heat They are probably also the main location where new continental crust is formed, the so-called ‘subduction factoiy’ About 400f modern subduction zones on Earth are intra-oceanic. These subduction systems are generally simpler than those at continental margins as they commonly have a shorter history of subduction and their magmas are not contaminated by ancient sialic crust. They are therefore the optimum locations for studies of mantle processes and magmatic addition to the crust in subduction zones. This volume contains a collection of papers that exploit the relative simplicity of intra-oceanic subduction systems to provide insights into the tectonic, magmatic and hydrothermal processes associated with subduction.

Description / Table of Contents: The 32 research papers in this volume examine the mode and nature of igneous, metamorphic, tectonic, sedimentological and biological processes associated with the evolution of ophiolites in Earth's history. Divided into six sections, the book presents a wealth of new data and syntheses from ophiotites around the world. Introductory chapters review the distribution of ophiolites in space and time and present a synoptic discussion on their importance in Earth history. Papers in the second section present diverse data from Tethyan ophiolites and provide refined geodynamic models for their evolution. The following two sections present case studies documenting magmatic, metamorphic and tectonic processes in ophiolite genesis and hydrothermal and biogenic alteration of fossil oceanic crust. Mechanisms of ophiolite emplacement are explored in Section V with a focus on the Semail massif (Oman). The last section examines the regional occurrence and geodynamic significance of ophiolite belts on different continents. The book reflects the contemporary work of the international community in a most up-to-date treatment of process-oriented questions on the evolution of ophiolites.

Description / Table of Contents: This book provides incentives for further development of sustainable fuel cycles through a novel and interdisciplinary approach to an Earth science-related topic. The main focus is on geochemical concepts in immobilizing, isolating or neutralizing waste derived from energy production and consumption. The book also addresses the issue of using some types of energy-derived waste as alternative raw materials. Moreover, it highlights research on how certain wastes can be used for energy production, an increasingly important aspect of modern integrated waste management strategies. The main objectives are to: (a) identify the most serious environmental problems related to various types of power generation and associated waste accumulation; (b) present strategies, based on natural analogue materials, for the immobilization of toxic and radioactive waste components through mineralogical barriers; (c) discuss modern procedures for reuse of waste or certain waste components; and (d) review the importance of geochemical modelling in describing and predicting the interaction between waste and the environment.

Description / Table of Contents: Reservoir geochemistry can throw light on the origin of petroleum reservoir fluidheterogeneities at a variety of spatial and temporal scales. This information can be usedto understand the formation and performance of petroleum accumulations, and is avaluable tool for exploration, development and productionstrategies. Key topics covered in this book include: analyticalmethods for the determination of fluid compositionalheterogeneity; physical, chemical and numerical models forinterpreting compositional differences in terms of basin historyand reservoir connectivity; and application case studies. There is now a significant potential for a new wave ofdevelopment focused on component concentrations and amore evolutionary chemical model of reservoired petroleum.When coupled with integrative utilitarian reservoir charge/mixing/production numericalmodels, reservoir geochemistry can provide one of the most significant advances inexploration and production during the 21st century.

Description / Table of Contents: Carbon dioxide (CO 2) is the main compound identified as affecting the stability of the Earth's climate. A significant reduction in the volume of greenhouse gas emissions to the atmosphere is a key mechanism for mitigating climate change. Geological storage of CO 2, or the injection and long-term stabilization of large volumes of CO 2 in the subsurface in saline aquifers, in existing hydrocarbon reservoirs or in unmineable coal seams, is one of the more technologically advanced options available. A number of studies have been carried out and are reported here. They are aimed at understanding the safety, physical and chemical behaviour and long-term fate of CO 2 when stored in geological formations. Until efficient, alternative energy options can be developed, geological storage of CO 2, the subject of this volume, provides a mechanism to reduce carbon emissions significantly whilst continuing to meet the global demand for energy.

Description / Table of Contents: Research into the orogenic processes that shaped the continental crust of Europe has a long-standing tradition. Why the need to quantify and model? It is not just satisfactory to identify subduction zones, accretionary prisms, island arcs, extensional collapse and other standard items of the geodynamic menu. Such interpretations need to be quantified: extent and composition of subducted crust, angle and speed of subduction, amount and composition olmelts produced, heat sources for metamorphism. All such interpretations have to conform to first principles, and also to stand the test of quantitative balancing - a concept first developed for the conservation of length or volume in tectonic cross sections. Also in other fields, the correlation of causes and effects and the internal consistency of dynamic models requires a numerical approach. The present volume combines review articles with reports on recent progress in an attempt to address these aims. There is a foldout map of the region, which locates the main areas of outcrop and tectono-stratigraphic units, and a reassesment of the Palaeozoic time scale permits correlation of tectonic, metamorphic and magmatic events with the sedimentary record of the upper crust.

Description / Table of Contents: Over long periods of time the tectonic evolution of the solid Earth has been recognized as the major control on the development of the global climate system. Tectonic activity acts in one of two different ways to influence regional and global climate: (i) through the opening and closing of oceanic gateways and its effect on the circulation patterns in the global ocean; (ii) through the growth and erosion of orogenic belts, resulting in changes in oceanic chemistry and disruption of atmospheric circulation. The Arabian Sea region has several features that make it the best area for studies of climate and palaeoceanographic responses to tectonic activity, most notably in the context of the South Asian monsoon and its relationship to the growth of high topography in the adjacent Himalayas and Tibet. The Tectonic and Climatic Evolution of the Arabian Sea Region brings together a collection of recent studies on the area from a wide group of international contributors. The paper range from high resolution, Holocene palaeoceanographic studies of the Pakistan margin to regional tectonic reconstructions of the ocean basin and surrounding margins throughout the Cenozoic. Marine geophysics, stratigraphy, isotope chemistry and neotectonics come together in a multidisciplinary approach to the study of interactions of land and sea. while much work remains to be done to understand fully the tectonic and climatic evolution of the Arabian Sea, a great deal has been achieved since the last major review, as detailed in the 26 contributions. This volume is essential reading for palaeoceanographers, sedimentologists and geophysicists. It will also be interest to structural geologists and those working in the petroleum industry.

Description / Table of Contents: The study of biodiversity through geological time provides important information for the understanding of diversity patterns at the present day. Hitherto, much effort has been paid to studying the mass extinctions of the Phanerozoic but the research emphasis has now changed to focus on what occurred between these spectacular catastrophic events. After the Cambrian ‘explosion’ of marine organisms with readily preservable skeletons, there have been two intervals when life radiated dramatically — the Ordovician Period, and the mid-Mesozoic-Cenozoic eras. These intervals saw a fundamental reorganization of biodiversity on a hierarchy of biogeographical scales. The size of these diversity increases and their probable causes are topics of intense debate, and there is an intriguing link between the dispersal of continents, changing climates and the proliferation of life. The papers in this volume are written by palaeontologists, biogeographers and geologists addressing the highly topical field of palaeobiodiversity in the context of the Earth’s changing geography. Palaeobiogeography and Biodiversity Change: the Ordovician and Mesozoic-Cenozoic Radiations illustrates many aspects of the two great episodes of biotic radiation and shows how long periods of time and plate tectonic movements have a fundamental influence on the generation and maintenance of major extant biodiversity patterns. The volume will be of interest to professional palaeontologists, biologists and geologists, as well as to students in earth and biological sciences.

Description / Table of Contents: This volume is a collection of papers on the history of twentieth century geology, of which eight were presented at a Symposium organized by the International Commission on the History of Geological Sciences (INHIGEO) for the International Geological Congress at Rio de Janeiro in 2000. The book offers a conspectus of selected developments of twentieth century geology. It has grown from largely a field discipline, chiefly concerned with rocks at the Earth's surface, to one that extends to the planet's interior, and to space beyond. New ideas, instruments, and techniques have extended the scope of earth science to the macro and the micro. Theories abound. One paper raises some of the social and political problems faced by modern geology. The volume is intended as a prolegomenon to some future synthetic understanding of twentieth century earth sciences. It should appeal to a wide range of geoscientists and historians of science.

Description / Table of Contents: Sustainable development of groundwater resources is a key environmental and social issue for the future. To manage groundwater resources efficiently it is necessary to include protection of springs, river flows and water levels dependent on groundwater discharges, while concurrently maintaining abstractions for water supply and economic benefit. Obtaining this balance between human and environmental needs, and protecting valuable groundwater resources from over-exploitation and pollution, presents a challenge to hydrogeologists that is reflected in the approaches and case studies contained in this volume. This volume should be of interest to researchers, regulators and practitioners in hydrogeology as well as postgraduate students following courses in hydrogeology, water resources engineering and environmental management.

Description / Table of Contents: There is an increasing trend in the Earth sciences towards the integration of many subdisciplines. The sedimendatry basin, is a fundamental focal point of many studies, which as a consequence often neglects the complimentary drainage basin or catchment. Sedimentary basins provide a record of Earth history, reflecting the geographical, lithological, oceanographic and ecological development through the rock record. Drainage basins in comparison record ephemeral landscape evolution, where topography is eroded and provides the flux of sediment to the basin. The basin fill reflects the sediment flux from the hinterland and provides evidence of the dynamic geomorphic processes. In context the drainage system and sedimentary basin can be regarded as a 'production line' with sedimentary record giving valuable insight into long-term landscape evolution and geomorphological processes illuminating the evolution of sedimentary basins. This volume assesses the current position of understanding sediment supply to basins with the integration of the many sub-disciplines in the Earth sciences. It documents a mix of hinterland and sedimentary basin studies with a gradation from orogenic belts to the deep marine. The authors represent a wide spectrum of Earth scientist, with leaders in the science providing review papers and new-directive papers in their field of specialization.

Description / Table of Contents: In a world of increasingly rapid technological and economic development, sea-level rise, and possible global climate change, central tasks facing the coastal and estuarine manager are to predict and manage change, undertaken against a background of constantly moving goalposts. There is an urgent need for a much better framework of background environmental data and more effective and reliable management tools, founded on sound scientific understanding, which can provide necessary guidance and the basis for policy formulation. Although these needs have been recognized, and some progress has been made in the past few years, an adequate suite of such management tools and frameworks for environmental monitoring is still some way off. The broad selection of papers included in this volume reflects the wide range of research currently being undertaken in coastal and estuarine environments, but underlines the fact that there are still significant gaps in understanding and major needs for further research which crosses traditional disciplinary boundaries. This volume brings together the results of recent research of sedimentologists, geomorphologists, archaeologists, engineers and others, expounding their methods and concerns, and identifying further areas where future joint work might be fruitful.

Description / Table of Contents: The Grès d′Annot Formation of SE France constitutes a classic and outstanding example of a sand-rich turbidite system controlled by synsedimentary tectonics, and has often been used as an outcrop analogue for deep-water hydrocarbon reservoirs. Over the last 10 years, research efforts by different academic and industrial teams have led to important reappraisals of prevailing ideas on the Gres d′Annot, particularly on the nature and controlling factors of the depositional processes, the small-scale architecture and sequence organization of the deposits, the tectonic regime of the basin and its impact on palaeogeography, and the interaction between sediment gravity flows and basin-floor topography. This volume offers a multidisciplinary overview and draws up the ′state-of-the-art′ of scientific knowledge on this influential turbidite system. Complementary aspects are covered, from structural geology, sedimentology and sequence stratigraphy, to modelling of sedimentary processes and architectures, geochemistry, reservoir characterization, seismic modelling and uses as analogues for deep-marine hydrocarbon fields. This book will be of use to both academic researchers (geologists and geophysicists) and industry professionals dealing with the characterization and modelling of deep-water sediments.

Description / Table of Contents: Forensic geoscience is an increasingly important sub-discipline within geoscience and forensic science. Although minerals, soils, dusts and rock fragments have been used as only begun to be recognized in the last ten years or so. The police and other investigative bodies are keen to encourage such developments in the fight against crime, particularly since many criminals show a high level of forensic awareness with regard to evidence such as fingerprints, blood and other body fluids. The papers in this volume illustrate some of the main principles, techniques and applications in current forensic geoscience, covering research and casework in the UK and internationally. The techniques described range from macro-scale field geophysical investigations to micro-scale laboratory studies of the chemical and textural properties of individual particles. In addition to forensic applications, many of these techniques have broad utility in geological, geomorphological, soil science and archaeological research.

Description / Table of Contents: This volume is a state of the art look at our understanding of joint development in the crust. Answers are provided for such questions as the mechanisms by which joints are initiated, the factors controlling the path they follow during the propagation process, and the processes responsible for the arrest of joints. Many of the answers to these questions can be inferred from the geometry of joint surface morphology and joint patterns. Joints are a record of the orientation of stress at the time of propagation and as such they are also useful records of ancient stress fields, regional and local. Because outcrop and subsurface views of joints are limited, statistical techniques are required to characterize joints and joint sets. Finally, joints are subject to post-propagation stresses that further localize deformation and are the focus for the development of new structures.

Description / Table of Contents: This volume explores geological boundaries in time and space using palynology and micropalaeontology. Boundaries produce distinct signatures in the micropalaeontological record. Diffuse or sharp, gradual or abrupt, boundaries can tell us much about the response of biotic systems to environmental change in both marine and terrestrial realms. Different microfossil groups and geological contexts require their own approaches, definitions and considerations of boundaries. The papers in this compilation capture the current range of thinking on the methodology of boundary identification from biostratigraphical, ecological and palaeoenvironmental perspectives. Contributions span the Cambrian to Miocene and feature many fossil groups (including pollen, dinoflagellates, foraminifera, ostracodes, conodonts, and diatoms). With a strong Canadian and North American focus, the volume also includes contributions from Poland, Egypt, Belgium, Argentina and the United Kingdom.

Description / Table of Contents: From the 1960s onwards, the Old Red Sandstone of both borders of the Atlantic Ocean has acted as a test-bed for the development of new ideas on the interpretation of fluvial, lacustrine and aeolian sedimentary rocks, and the investigation of tectonically-active basins. Much of the earlier reconnaissance work is now being reviewed in the light of further detailed field study, along with new developments in the understanding of the biostratigraphy, palaeobiology, geochronology, pedogenesis and tectonics. Three general papers review recent work on the stratigraphical and chronological analysis of the Late Silurian, Devonian and Early Carboniferous strata, and summarize present understanding of the tectonics of the basins. These are then followed by twenty-seven contributions covering new work in Eastern USA, Canada, Ireland, Britain, Norway, Greenland and Spitsbergen.

Description / Table of Contents: This volume is a collection of papers, with an introduction, concerning the consequences of organism-environment interactions for modern and ancient carbonate platform systems. They arise from the 1999 Lyell Meeting on ‘Organism-Environment Feedbacks in Carbonate Platforms and Reefs’. The papers presented here provide an integrated view of carbonate platforms, emphasizing dynamic interactions at all hierarchical levels and revealing the limitations of uniformitarian analogy in biotically influenced sedimentary systems. Selected case studies from around the world illustrate aspects ranging from the genesis of growth fabrics to changing patterns of carbonate platform development. The text will be of interest to sedimentologists, palaeontologists and marine ecologists alike.

Description / Table of Contents: The study of sediments and sedimentary basins in terms of their tectonic environment requires a multidisciplinary approach and has increasingly drawn both techniques and objectives from fields outside sedimentology. The application of different theoretical, experimental and empirical resources provided by structural geology, geochemistry, geophysics, scale modelling, and field geology, complement sedimentological methods, with the combined aim of achieving a deeper understanding of the origins, evolution and significance of sedimentary sequences in terms of their tectonic history. Studies presented in this volume range across a wide spectrum from the analysis of sedimentary sequence architecture at basin scale down to the chemical properties of individual grains, and include studies from a range of tectonic settings. The volume will be of interest to those involved with, or contemplating, studies involving the linkages between tectonics and sedimentation, as well as a wider audience to whom the results of such studies may provide fresh insight.

Description / Table of Contents: This volume focuses on Late Mesoproterozoic to early Cambrian events related to Gondwana assembly and break up. The nineteen papers provide a comprehensive review including advanced knowledge and new data from all critical areas of East Gondwana. The recent knowledge of the evolution of East Gondwana, which was regarded as an integral part of the Mesoproterozoic supercontinent Rodinia, is the major theme of the volume, which is reinforced by highlighting this radical and new understanding of the evolution of this region. This volume is of use as both a text and reference book for Earth Science postgraduates, and should appeal worldwide to professional geologists with an interest in Rodinia, Gondwana and that important transition from the Proterozoic to the Phanerozoic Earth.

Description / Table of Contents: This book examines the process and patterns of glacier-influenced sedimentation on high-latitude continental margins and the geophysical and geological signatures of the resulting sediments and landforms. It contains a range of papers concerning modern and glacially-influenced sedimentation in high-latitude areas from both hemispheres, many of which discuss the relationship between glacier dynamics and the sediments and landforms preserved in the glacimarine environment This volume will be of interest to those in academia and industry working in the broad fields of glacimarine environments, the development of high-latitude margins and marine geology and geophysics

Description / Table of Contents: As an outcome of the European Science Foundation scientific programme, GEODE, on geodynamics and ore deposit evolution, this book examines the underlying geodynamic processes that lead to the formation of ore deposits in order to discover what controls the timing and location of major ore deposits in an evolving orogen. A collection of 19 research papers examines various aspects of ore genesis in the context of the geodynamic processes occurring within an evolving orogen. Although the majority of papers relate to Europe, their findings have a global significance for metallogenesis. The book will be of interest to all those involved in research or mineral exploration concerned with metallogenesis. In addition, ore deposits provide new evidence about magmatism associated with transient, rapid changes in plate motions and subduction processes in unusual tectonic settings, and are therefore of interest to those involved in both the magmatic and tectonic processes of orogenesis.

Description / Table of Contents: The weathering of historical buildings and, indeed, of monuments and sculptures of natural stone is a problem that has been encountered for hundreds of years. However, a dramatic increase in deterioration in the structure of our built heritage has been observed during the past century. To understand the complex interaction that the stone in a building suffers with its near environment (the building) and the macro environment (the local climate and atmospheric conditions) requires an interdisciplinary approach and the application of many different theoretical, experimental and empirical resources provided by the geosciences, chemistry, material sciences, biology and construction engineers. The protection of our architectural heritage has both cultural and historical importance, as well as substantial economic and ecological value. Large sums of money are being spent world-wide on measures for the preservation of monuments and historical buildings. Optimization of damage analysis procedures and damage process controls, as well as the development of monitoring and early warning systems for damage prevention, is needed. The past several decades has seen an unprecedented level of research activity in this area, the results of which are often difficult to access. This volume is intended to provide an integrated approach to the study of the deterioration of geomaterials, making the research available to a wide international audience. Natural Stone, Weathering Phenomena, Conservation Strategies and Case Studies comprises thirty chapters divided into six sections: weathering of natural building stones; weathering processes; fabric dependence of physical properties; biodeterioration; quality assessment and conservation of stones; and environmental conditions. Review articles are combined with reports on recent progress in the various research fields, authored by a comprehensive team of international contributors. The volume will be of interest to all those involved in the protection of our built heritage, particularly geoscientists, material scientists, construction engineers, architects and stone conservators.

Description / Table of Contents: This volume focuses on magmas and cryospheres on Earth and Mars and is the first publication of its kind to combine a thematic set of contributions addressing the diverse range of volcano-ice interactions known or thought to occur on both planets. Understanding those interactions is a comparatively young scientific endeavour, yet it is vitally important for a fuller comprehension of how planets work as integrated systems. It is also topical since future volcanic eruptions on Earth may contribute to melting ice sheets and thus to global sea level rise. Papers included here are likely to influence the choice of sites for future Mars missions in exobiologically important areas. On Earth, snow and ice are widespread, not only in extensive icecaps but also as alpine glaciers at high elevations in tropical regions. By contrast, Mars today is an arid volcanic planet with only small polar ice-caps although an abundance of water is believed to be trapped in the cryolithosphere. It is also thought that the planet may have sustained extensive frozen oceans early in its history. The presence of a former hydrosphere, a cryosphere and coincident volcanism thus make Mars the likeliest prospect for the first discoveries of life away from Earth. Much research has assumed that terrestrial volcano-ice systems are plausible analogues for putative Martian examples, but until mankind finally sets foot on Mars, there is no simple test for that assumption. Our hope is that the knowledge presented here will stimulate research among planetary geologists in this exciting, rapidly expanding field for many years to come.

Description / Table of Contents: The motion and deformation of rocks are processes of fundamental importance in shaping the Earth, from outer crustal layers to the deep mantle. Reconstructions of the evolution of the Earth therefore require detailed knowledge of the geometry of deformation structures and their relative timing, of the motions leading to deformation structures and of the mechanisms governing these motions. This volume contains a collection of 22 papers on field, experimental and theoretical studies that add to our knowledge of these processes. They are a mixture of review papers oh selected topics in the field of structural geology and tectonics and papers on current issues and new techniques and are grouped into four themes: • The effect of fluids on deformation • The interpretation of microstructures and textures • Deformation mechanisms and rheology of crust and upper mantle minerals • Crust and lithosphere tectonics The volume will appeal to researchers in the fields of structural geology and tectonophysics, both in academia and industry.

Description / Table of Contents: Palaeozoic Amalgamation of Central Europe summarizes recent research designed to clarify the timing, geometry and processes by which discrete terranes of Central Europe became amalgamated during the Palaeozoic Era. The area studied extends from the southern North Sea to Central Poland along the Trans-European Suture Zone, covering much of Germany, Denmark, Belgium, the Czech Republic and Poland. The 16 papers within the volume are divided into five sections: biostratigraphic/provenance evidence; isotopic constraints; petrological and geochemical evidence; structural evolution; seismic traverses and deep crustal structure. The first section contains papers summarizing continent-specific micropalaeontological and sediment provenance information backing current debates about microcontinent derivation and timing of their accretions to the proto-European continent, Baltica. The section on isotopic constraints discusses the use of isotopic dating to constrain the timing of accretions of rock units exposed in the northern Bohemian Massif, while the following section has more detailed studies of metamorphosed ophiolitic complexes adjoining palaeosutures in the same area. The two papers on the structural evolution of the area contrast a detailed review of the structural evolution of the Sudetes, with a broader, more regionally based hypothesis for the structural evolution of all Central Europe. The final section discusses models based on extensive seismic traverses in contrasting parts of the area - Belgium, the southern North Sea and Poland. This wide-ranging study thus encapsulates the most up-to-date ideas on the Palaeozoic amalgamation of Central Europe from the leading international researchers in the field. The volume will be of interest to those earth scientists in industry and academia with a broad-based interest in the construction of the European continent, primarily biostratigraphers, geophysicists, structural geologists and geochemists.

Description / Table of Contents: This volume contains a series of papers that cover a wide range of aspects, including geophysics, structure and tectonics, atmosphere, origin of life, biosphere, deep mantle geochemistry, early oceans, microbial ecology, on the development of the Earth in the first 2000 Ma of its history.The aim of this publication is to facilitate future discussions and understanding of this area of research. This book is divided into three parts: • Geophysical and petrological constraints on Archaean lithosphere • Models of cratonic evolution and modification • Constraints on the Archaean environment Subjects covered include the chemical and biological controls on the atmosphere and oceans, early controls on the carbon cycle and photosynthesis, petrologic, isotopic, tectonic and seismic evidence for the composition and structure of Archaean lithosphere. This volume should be of interest to geologists and geophysicists who work on the Archaean, and students at all levels.

Description / Table of Contents: This book is a collection of keynote reviews and detailed case-studies covering the principal areas of active research and state-of-the-art industrial practice in the field of mine water management. It addresses both issues of water quantity (such as the impact of Iongwall mining on the piezometry and hydraulic properties of overlying aquifers) and water quality (spanning an array of sites from deep coal mines to open-pit base metal mines), as well as a wealth of hybrid, integrated studies in which hydrogeological and geochemical aspects are considered (and managed) together. The papers presented in this book are intended for practicing geologists and engineers involved in the management of active and abandoned mine sites all over the world. It is also of interest to academic geoscientists and students with interests in low-temperature aqueous geochemistry and the hydrogeology of complex, quasi-karstic groundwater flow systems.

Description / Table of Contents: The North Atlantic Igneous Province has been the subject of extensive scientific investigation over the past thirty years, with a wide field of knowledge being accumulated. Recently, recognition of the potential role of Large Igneous Provinces in affecting ocean and atmosphere systems and biotic evolutionary pathways has lead to increased interest in this province. This has been further stimulated by the expansion in the search for oil and gas in Mesozoic and Tertiary sediments along the NE Atlantic Margin. An improved understanding of the interaction between igneous and sedimentary processes is vital for the identification of potential hydrocarbon resources. The regions covered include continental margin Norway, east and west Greenland, the Faroe-Shetland Basin and the Faroe Islands themselves. The papers in this book contain new data and interpretations of North Atlantic Igneous Province magmatic processes, rift evolution, tectonics, stratigraphy (chemostratigraphy, biostratigraphy, seismic and isotope stratigraphy) and sediment dispersal. Many of the papers adopt a multidisciplinary approach to tha analysis and interpretation of complex volcanic and sedimentary sequences. These new data, and the reviews and compilations of existing data provide the reader with access to current research directions in North Atlantic Igneous Province geology.

Description / Table of Contents: Northwest Europe has undergone repeated episodes of exhumation (the exposure of formerly buried rocks) due to such factors as post-orogenic unroofing, rift-shoulder uplift, hotspot activity, compressive tectonics, eustatic sea-level change, glaciation and isostatic readjustment. The main observational legacy of this exhumation around the North Atlantic is preserved in the comparatively young (Mesozoic and Cenozoic) geological record of this region. Despite a rapid increase in the understanding of the exhumation of this area, there are still many unknowns: the relative intensity of the various phases and their geographical variation; mechanisms of uplift; primary causes of exhumation. Tied to these problems is the larger-scale question of whether the circum-North Atlantic is unique or whether its behaviour is typical for passive margins. There have been several attempts in recent years to bring together researchers to address these questions, but these have often focused on one particular geographical area or one particular exhumation phase. Before an integrated story can emerge, disciplines that have traditionally remained apart need to come together: geomorphology and offshore seismic interpretation; Palaeogene and Neogene studies; Scandinavian and British-Irish research schools. This volume represents a first step in this direction by providing an inter-disciplinary set of studies over a wide latitudinal range of the NW European margin. The studies presented here are based on a variety of techniques that have been employed to address the main concerns of North Atlantic exhumation history, including timing, mechanisms and the sedimentary response of the continental margin. The 25 papers presented in this volume have