ALBERT

Description / Table of Contents: Profiles of particulate and dissolved 234Th (t1/2=24.1 days) in seawater and particulate 234Th collected in drifting traps were analyzed in the Barents Sea at five stations during the ALV3 cruise (from June 28 to July 12, 1999) along a transect from 78°15′N–34°09′E to 73°49′N–31°43′E. 234Th/238U disequilibrium was observed at all locations. 234Th data measured in suspended and trapped particles were used to calibrate the catchment efficiency of the sediment traps. Model-derived 234Th fluxes were similar to 234Th fluxes measured in sediment traps based on a steady-state 234Th model. This suggests that the sediment traps were not subject to large trapping efficiency problems (collection efficiency ranges from 70% to 100% for four traps). The export flux of particulate organic carbon (POC) can be calculated from the model-derived export flux of 234Th and the POC/234Th ratio. POC/234Th ratios measured in suspended and trapped particles were very different (52.0±9.9 and 5.3±2.2 μmol dpm−1, respectively). The agreement between calculated and measured POC fluxes when the POC/234Th ratio of trapped particles was used confirms that the POC/234Th ratio in trap particles is representative of sinking particles. Large discrepancies were observed between calculated and measured POC fluxes when the POC/234Th ratio of suspended particles was used. In the Barents Sea, vertical POC fluxes are higher than POC fluxes estimated in the central Arctic Ocean and the Beaufort Sea and lower than those calculated in the Northeast Water Polynya and the Chukchi Sea. We suggest that the latter fluxes may have been strongly overestimated, because they were based on high POC/234Th ratios measured on suspended particles. It seems that POC fluxes cannot be reliably derived from thorium budgets without measuring the POC/234Th ratio of sediment trap material or of large filtered particles.

Description / Table of Contents: This handbook is for any educator teaching a topic that includes data analysis or computation in order to support learning. It is not just for educators teaching courses in engineering or science, but also data journalism, business and quantitative economics, data-based decision sciences and policy, quantitative health sciences, and digital humanities. It aims to provide an entry point, and a broad overview of Jupyter in education. Whether you are already using Jupyter to teach, you have found learning materials built on Jupyter that piqued your curiosity, or have never heard of Jupyter, the material in this open book can empower you to use this technology in your teaching. Project Jupyter is a broad collaboration that develops open-source tools for interactive and exploratory computing. The tools include: over 100 computer languages (with a focus on Python), the Jupyter Notebook, JupyterHub, and an ecosystem of extensions contributed by a large community. The Jupyter Notebook has exploded in popularity since late 2014, fueled by its adoption as the favorite environment for doing data science. It has also grown as a platform to use in the classroom, to develop teaching materials, to share lessons and tutorials, and to create computational stories. Notebooks are documents containing text narratives with images and math, combined with executable code (many languages are supported) and the output of that code. This marriage of content and code makes for a powerful new form of data-based communication. Educators everywhere are adopting Jupyter for teaching. Educators newly adopting Jupyter can be overwhelmed by having to navigate the ecosystem of tools and content. They could study many examples, or consume a myriad of blog posts and videos of talks to distill the patterns of good practices and technical solutions to serve their students best. Several early adopters, having much experience to share, decided to begin collecting this know-how, and share open documentation about using Jupyter for teaching and learning. The result is this open book: a living document that captures the experiences of community members using Jupyter in education. The Jupyter Community Workshop in Washington, DC (November 2018) began that process, with a book sprint aimed at producing the first version of this handbook. The collaboratively written book consolidates explanations and examples covering key topics, including: what is Jupyter, how to try Jupyter, sharing notebooks with students, locally installing Jupyter, cloud offerings, finding example notebooks, writing lessons in Jupyter, making collections for a course, exporting to other formats with nbconvert, writing textbooks with Jupyter, using Binder and JupyterHub, making assignments and auto-grading, making online courses, teaching with Jupyter in the classroom, active learning and flipped learning pedagogies with Jupyter, and guiding learners to create their own content in Jupyter. This open handbook will grow to encompass all you need to know about Jupyter in teaching and learning.

Description / Table of Contents: "Earthquakes and Animals places in front of the reader the simple laboratory evidence of the behavior of animals, plants and objects when they are subjected to intense electromagnetic pulses - of the kind created by rocks under stress before an earthquake. In many cases they behave in ways that have been recorded for centuries - and are still reported today - as earthquake-related." "Written for both the general public and scientists, Earthquakes and Animals demonstrates, using many experiments, that the old earthquake legends are probably rare natural phenomena. It also adds tantalisingly to the science of earthquake forecasting and cautiously suggests a legitimate new field of study - Electromagnetic Seismology."--BOOK JACKET

Description / Table of Contents: 'The Diversity Scorecard' is designed to provide step-by-step instructions, worksheets and examples to help diversity executives and managers analyze and track the impact of their diversity initiatives to mobilize the organization for strategic culture change. Diversity is not a program; it is a systemic process of organizational change that requires measurement for organizational improvement and success. Measuring the progress and results of diversity initiatives is a key strategic requirement to demonstrate its contribution to organizational performance. Diversity executives, professionals and managers know they must begin to show how diversity is linked to the bottom-line in hard numbers or they will have difficulty maintaining funds, gaining support, and obtaining resources to generate progress. Many organizations collect some type of diversity-related data today, even if it focuses only on Affirmative Action statistics. "The Diversity Scorecard" focuses on tools and techniques to make sure diversity professionals are collecting and measuring the right type of data that will help ensure the organization"s success both now and in the future. This book helps the reader spend some time thinking about what they currently measure and adding new measures to a database to track progress towards their diversity vision. The basic premises of this book are that it is important to develop measures that focus on the past, present, and future; and that measures need to consider the needs of the organization"s diverse workforce, its work climate, diverse customers, the community, and shareholders. Part I of "The Diversity Scorecard" identifies the need for diversity measurement highlighting a business case for diversity and providing an introduction to diversity measurement. Part II of the book outlines the diversity return on investment (DROI) process taking you through step-by-step processes and techniques. Part III teaches you how to use measures in six key categories - Diversity Leadership Commitment, Workforce Profile Representation, Workplace Climate, Learning & Growth, Diverse Customer / Community Partnerships, and Financial Impact - to build a diversity scorecard that is aligned and linked with the business strategy of the organization. Finally, in Part IV, Dr. Hubbard discusses implementation issues involving strategic change procedures and techniques to avoid the pitfalls inherent in a diversity-based cultural transition process.

Description / Table of Contents: On September 10, 1996, The United Nations General Assembly adopted the Copmprehensive Nuclear-Test-Ban Treaty (CTBT), prohibiting nuclear explosions worldwide, in all environments. The treaty calls for a global verification system, including a network of 321 monitoring stations distributed around the globe, a data communications network, an international data center (IDC), and on-site inspections, to verify compliance. This volume presents certain recent research results pertaining on methods used to process data recorded by instruments of the International Monitoring System (IMS) and addressing recording infrasound signals generated by atmospheric explosions. Six papers treating data processing provide an important selection of topics expected to contribute to improving our ability to successfully monitor a CTBT. Five papers concerning infrasound include descriptions of ways in which that important research area can contribute to CTBT monitoring, the automatic processing of infrasound data, and site conditions that serve to improve the quality of infrasound data.

Description / Table of Contents: In the last decade of the 20th century, there has been great progress in the physics of earthquake generation; that is, the introduction of laboratory-based fault constitutive laws as a basic equation governing earthquake rupture, quantitative description of tectonic loading driven by plate motion, and a microscopic approach to study fault zone processes. The fault constitutive law plays the role of an interface between microscopic processes in fault zones and macroscopic processes of a fault system, and the plate motion connects diverse crustal activities with mantle dynamics. An ambitious challenge for us is to develop realistic computer simulation models for the complete earthquake process on the basis of microphysics in fault zones and macro-dynamics in the crust-mantle system. Recent advances in high performance computer technology and numerical simulation methodology are bringing this vision within reach. The book consists of two parts and presents a cross-section of cutting-edge research in the field of computational earthquake physics. Part I includes works on microphysics of rupture and fault constitutive laws, and dynamic rupture, wave propagation and strong ground motion. Part II covers earthquake cycles, crustal deformation, plate dynamics, and seismicity change and its physical interpretation. Topics in Part II range from the 3-D simulations of earthquake generation cycles and interseismic crustal deformation associated with plate subduction to the development of new methods for analyzing geophysical and geodetical data and new simulation algorithms for large amplitude folding and mantle convection with viscoelastic/brittle lithosphere, as well as a theoretical study of accelerated seismic release on heterogeneous faults, simulation of long-range automaton models of earthquakes, and various approaches to earthquake predicition based on underlying physical and/or statistical models for seismicity change.

Description / Table of Contents: Underpinning international efforts to combat climate change are a series of actions being taken by developed countries' governments to mitigate emissions of greenhouse gases. This volume details more than 200 new policies and measures that were taken in the year 2000 to address energy-related emissions in IEA member countries. Actions are listed for each of the 26 IEA Member countries under five major headings: fiscal policy, tradable permits, regulatory instruments and voluntary approaches, R&D policy, and policy processes. In addition, policies are classified according to energy source and end use.

Description / Table of Contents: Im Rahmen der 74. Jahrestagung der Paläontologischen Gesellschaft, die 2004 zum vierten Mal in Göttingen stattfand, wurden sechs Exkursionen in die nähere Umgebung Göttingens durchgeführt sowie Workshops zu Geo-Histologie, Öffentlichkeitsarbeit und Ostrakoden angeboten. Der vorliegende Exkursionsführer und Workshop-Begleiter ist mit zahlreichen Abbildungen und Farbseiten ausgestattet. Er bietet zur regionalen Geowissenschaft Niedersachsens und zu den genannten Workshop-Themen aktuelle und fundierte Informationen.

Description / Table of Contents: Papers from the Research Workshop on Inherently Parallel Algorithms in Feasibility and Optimization and Their Applications, held in Haifa, Israel, Mar. 13-16, 2000

Description / Table of Contents: With the publication of the present volume, the Handbook of the History of Logic turns its attention to the rise of modern logic. The period covered is 1685-1900, with this volume carving out the territory from Leibniz to Frege. What is striking about this period is the earliness and persistence of what could be called 'the mathematical turn in logic'. Virtually every working logician is aware that, after a centuries-long run, the logic that originated in antiquity came to be displaced by a new approach with a dominantly mathematical character. It is, however, a substantial error to suppose that the mathematization of logic was, in all essentials, Frege's accomplishment or, if not his alone, a development ensuing from the second half of the nineteenth century. The mathematical turn in logic, although given considerable torque by events of the nineteenth century, can with assurance be dated from the final quarter of the seventeenth century in the impressively prescient work of Leibniz. It is true that, in the three hundred year run-up to the Begriffsschrift, one does not see a smoothly continuous evolution of the mathematical turn, but the idea that logic is mathematics, albeit perhaps only the most general part of mathematics, is one that attracted some degree of support throughout the entire period in question. Still, as Alfred North Whitehead once noted, the relationship between mathematics and symbolic logic has been an "uneasy" one, as is the present-day association of mathematics with computing. Some of this unease has a philosophical texture. For example, those who equate mathematics and logic sometimes disagree about the directionality of the purported identity. Frege and Russell made themselves famous by insisting (though for different reasons) that logic was the senior partner. Indeed logicism is the view that mathematics can be re-expressed without relevant loss in a suitably framed symbolic logic. But for a number of thinkers who took an algebraic approach to logic, the dependency relation was reversed, with mathematics in some form emerging as the senior partner. This was the precursor of the modern view that, in its four main precincts (set theory, proof theory, model theory and recursion theory), logic is indeed a branch of pure mathematics. It would be a mistake to leave the impression that the mathematization of logic (or the logicization of mathematics) was the sole concern of the history of logic between 1665 and 1900. There are, in this long interval, aspects of the modern unfolding of logic that bear no stamp of the imperial designs of mathematicians, as the chapters on Kant and Hegcl make clear. Of the two, Hcgel's influence on logic is arguably the greater, serving as a spur to the unfolding of an idealist tradition in logic - a development that will be covered in a further volume, British Logic in the Nineteenth Century. Contents: Preface (D.M. Gabbay, J. Woods). List of Contributors. Leibniz's Logic (W. Lenzen). Kant: From General to Transcendental Logic (M. Tiles). Hegel's Logic (J.W. Burbidge). Bolzano as Logician (P. Rusnock, R. George). Husserl's Logic (R. Tieszen). Algebraical Logic 1685-1900 (T. Hailperin). The Algebra of Logic (V.S. Valencia). The Mathematical Turn in Logic (I. Grattan-Guinness). Schroder's Logic (V. Peckhaus). Peirce's Logic (R. Hilpinen). Frege's Logic (P. Sullivan). Index.

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: 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: 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: 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: World energy demand will rise by two thirds between now and 2030, and the world economy will falter if these energy supplies are not available. How much investment will be required to satisfy this need and can it be financed is looked into, in an attempt to quantify global energy investment needs, fuel-by-fuel and region-by-region. The global financial system has the capacity to fund the required investment, but are the conditions right? For some sectors and regions, the prospects are good. For others, the outlook is bleak. The total figure which emerges for the required global investment over 30 years is large - $16 trillion, but there are no claims that this will be validated in 30 years time. Policymakers perhaps will have failed if the energy economy has not been reshaped to make it more sustainable. Issues looked at by the World Energy Investment Outlook 2003 are global energy investment needs to 2030, financing global energy investment, as well as specifically oil, natural gas, coal, electricity and advanced technologies.

Description / Table of Contents: The widespread extension occured within the Variscan orogen and its northern foreland during late Carboniferous to Early Permian times. This was associated with magnetism and with a fundamental change, at the Westphalian-Stephanian boundary, in the regional stress field, coincident with the termination of orogenic activity and onset of dextral translation between North Africa and Europe. Rifting propagated across basement terranes with different ages and thermal histories. Most of the roft basins developed on relatively thin lithosphere; however, the highly magnetic Oslo graben initiated within the edge of a craton. Early stephanian regional uplift is contemporaneous with the onset of magmatism; inviting speculation that it might have been induced by a thermal anomaly within the upper mantle. The contributions to this volume suggest that the geodynamic setting in which magmatism occurred was complex, involving wrench tectonics, slab detachment, and delimination or thermal erosion of the base of the lithosphere.

Description / Table of Contents: ‘Commercial oil deposits in basement rocks are not geological “accidents” but are oil accumulations which obey all the rules of oil sourcing, migration and entrapment; therefore in areas of not too deep basement, oil deposits within basement rocks should be explored with the same professional skill and zeal as ccumulations in the overlying sediments’, Landes et al. (1960), AAPG Bulletin. Given that most OPEC countries are currently at or within 5% Production capacity, there is a growing need to look for ‘new oil’ and other hydrocarbons in non-traditional sources. While oil and gas fields in crystalline basement are still discovered mostly by accident, as shown in this book, such reservoirs can be very prolific, especially if the basement rock is highly faulted or fractured. The chapters in this volume cover a diverse range of topics related broadly to the theme of hydrocarbons in crystalline rocks, and challenge explorationists’ definition of basement rock, which needs to be less narrow and more responsive to new geological ideas.

Description / Table of Contents: Intraplate strike-slip deformation belts are common tectonic features, particularly at convergent plate boundaries, where they are produced by both oblique convergence and continental indentation. These lithosphere-scale structures, which also occur in other geodynamic environments such as passive margins, are characterized by complex structural architectures, by the occurrence of large earthquakes, and by the fast uplift and/or subsidence of localized crustal sectors. Intraplate strike-slip belts can also control the ascent and emplacement of deeply sourced magmas. In some cases, intraplate strike-slip belts link with oceanic fracture zones and transform faults, transferring transform shear from the ridges to the interior of the plates. This evidence has an important impact of the classical concept of transform faulting. This volume contains 13 papers from an international field of contributors. Studies of intraplate strike-slip deformation belts from Africa, Antarctica, Eurasia, North America and South America are included.

Description / Table of Contents: Applications of X-ray computed tomography in the geosciences / F. Mees, R. Swennen, M. Van Geet and P. Jacobs / Geological Society, London, Special Publications, 215, 1-6, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.01 --- Applications of high-resolution X-ray computed tomography in petrology, meteoritics and palaeontology / W. D. Carlson, T. Rowe, R. A. Ketcham and M. W. Colbert / Geological Society, London, Special Publications, 215, 7-22, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.02 --- Computed tomography in petroleum engineering research / S. Akin and A. R. Kovscek / Geological Society, London, Special Publications, 215, 23-38, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.03 --- Study of the microgeometry of porous materials using synchrotron computed microtomography / K. W. Jones, H. Feng, W. B. Lindquist, P. M. Adler, J. F. Thovert, B. Vekemans, L. Vincze, I. Szaloki, R. Van Grieken, F. Adams and C. Riekel / Geological Society, London, Special Publications, 215, 39-49, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.04 --- Porosity measurements of sedimentary rocks by means of microfocus X-ray computed tomography (μCT) / M. Van Geet, D. Lagrou and R. Swennen / Geological Society, London, Special Publications, 215, 51-60, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.05 --- Quantitative characterization of fracture apertures using microfocus computed tomography / K. Vandersteen, B. Busselen, K. Van Den Abeele and J. Carmeliet / Geological Society, London, Special Publications, 215, 61-68, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.06 --- Three-dimensional visualization of fractures in rock test samples, simulating deep level mining excavations, using X-ray computed tomography / E. Sellers, A. Vervoort and J. Van Cleynenbreugel / Geological Society, London, Special Publications, 215, 69-80, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.07 --- Geostatistics and the representative elementary volume of gamma ray tomography attenuation in rock cores / J. R. Vogel and G. O. Brown / Geological Society, London, Special Publications, 215, 81-93, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.08 --- Porosity and fluid flow characterization of granite by capillary wetting using X-ray computed tomography / Y. Géraud, F. Surma and F. Mazerolle / Geological Society, London, Special Publications, 215, 95-105, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.09 --- Direct imaging of fluid flow in fault-related rocks by X-ray CT / T. Hirono, M. Takahashi and S. Nakashima / Geological Society, London, Special Publications, 215, 107-115, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.10 --- Rock drying tests monitored by X-ray computed tomography — the effect of saturation methods on drying behaviour / B. Rousset-Tournier, F. Mazerolle, Y. Géraud and D. Jeannette / Geological Society, London, Special Publications, 215, 117-125, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.11 --- Characterization by X-ray computed tomography of water absorption in a limestone used as building stone in the Oviedo Cathedral (Spain) / V. G. Ruiz de Argandoña, A. Rodriguez-Rey, C. Celorio, L. Calleja and L. M. Suárez del Rio / Geological Society, London, Special Publications, 215, 127-134, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.12 --- Estimation of porosity and hydraulic conductivity from X-ray CT-measured solute breakthrough / S. H. Anderson, H. Wang, R. L. Peyton and C. J. Gantzer / Geological Society, London, Special Publications, 215, 135-149, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.13 --- Assessment of soil structure using X-ray computed tomography / H. Rogasik, I. Onasch, J. Brunotte, D. Jegou and O. Wendroth / Geological Society, London, Special Publications, 215, 151-165, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.14 --- 3D soil image characterization applied to hydraulic properties computation / J. F. Delerue, E. Perrier, A. Timmerman and R. Swennen / Geological Society, London, Special Publications, 215, 167-176, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.15 --- Evaluation of local porosity changes in limestone samples under triaxial stress field by using X-ray computed tomography / C. O. Karacan, A. S. Grader and P. M. Halleck / Geological Society, London, Special Publications, 215, 177-189, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.16 --- Monitoring void ratio redistribution during continuous undrained triaxial compression by X-ray computed tomography / P. R. Thomson and R. C. K. Wong / Geological Society, London, Special Publications, 215, 191-198, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.17 --- The use of X-ray computed tomography in the investigation of the settlement behaviour of compacted mudrock / M. A. O’Neill, A. K. Goodwin and W. F. Anderson / Geological Society, London, Special Publications, 215, 199-204, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.18 --- Industrial X-ray computed tomography studies of lake sediment drill cores / A. Flisch and A. Becker / Geological Society, London, Special Publications, 215, 205-212, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.19 --- Analysis of analogue models by helical X-ray computed tomography / G. Schreurs, R. Hänni, M. Panien and P. Vock / Geological Society, London, Special Publications, 215, 213-223, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.20 --- Preliminary microfocus X-ray computed tomography survey of echinoid fossil microstructure / S. R. Stock and A. Veis / Geological Society, London, Special Publications, 215, 225-235, 1 January 2003, https://doi.org/10.1144/GSL.SP.2003.215.01.21

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: Ireland is virtually encircled by sedimentary basins which developed in response to periods of rifting and thermal subsidence. These offshore basins have been the focus of intermittent phases of exploration since drilling of the first well in 1970 and, to date, 136 wells have been drilled. Most of the drilling so far has concentrated on structural traps, but recent exploration has begun to focus on a variety of stratigraphic traps, with greater emphasis on results obtained from studies of the Atlantic margin basins. The Petroleum Exploration of Ireland's Offshore Basins contains a set of 27 papers on a wide range of topics relating to recent exploration of the Irish offshore sedimentary basins. These papers address aspects of the structural and stratigraphic evolution, thermal history, petroleum systems, reservoir geology and sea-bed processes in the Irish offshore area. Although the main focus is on petroleum systems and those issues bearing on exploration risk, the exploration effort has yielded fundamental new insight into the wider development of starved passive continental margins. The volume will be of interest to oil industry explorationists and researchers focusing on NW European sedimentary basins and the evolution of the Irish Atlantic margin.

Description / Table of Contents: This volume describes the use of till geochemical and indicator mineral methods for mineral exploration in glaciated terrain of Canada. The principles and examples described in this volume wil have direct applications for exploration companies and prospectors exploring for diamonds, precious and base metals and uranium in glaciated parts of North America, northern Europe and Asia and mountainous regions of South America. The first two papers in this volume provide an introduction to glaciated terrain and the two styles of glaciation that have affected the world, continental glaciers in broad flat lying Shield areas and alpine glaciers in mountainous terrain. Sampling techniques are described next, followed by an introduction to the use of heavy minerals. Heavy mineral methodss have become an important exploration tool in glaciated terrain for gold and base metals and, in the last ten years, for diamonds. Lake sediments and biogeochemical methods are also included in this volume as a complement to geochemical and indicator mineral methods in glaciated terrain. A chapter on GIS has been included because data interpretation and display are important and essential parts of any regional or detailed geochemical survey. The remainder of the volume is case studies for the three main glaciated terrain tyes in Canada: Shield, Appalachia and Cordillera

Description / Table of Contents: The climate of the early Earth was probably very warm and has, in general, reduced since the Archean. However, it now seems that the world is about 0.6°C warmer than it was 100 years ago and estimates of the rate of global warming over the next century range from 0.16°C to 0.35°C per decade. Concurrently, global sea-level is predicted to rise from 2.4 to 10 cm per decade. These rates of change are much faster than those normally associated with the geological record, causing geologists and palaeontologists to reassess their data and their forecasts on rates of future change. With the current interest in global climatic change and, more specifically, with global warming, it is clear that palaeontologists have valuable information to provide on the impacts of past climatic change. This volume contains papers from an international array of such geologists and palaeontologists, showing how studies of micro- and macrofossils, plant and vertebrate fossils from a range of geological ages have contributed to our understanding of how climate affects both local and more widespread areas. The contributions are arranged in geological order, ranging from the Permo-Carboniferous to the post-glacial recovery of the last 18,000 years, with an emphasis on climate change during the last two million years, particularly in NW Europe. Climates: Past and Present will be of interest to palaeontologists, geologists and palaeoclimatologists who specialize in climatic reconstructions and any professionals enagaged in research into the geological aspects of climate change.

Description / Table of Contents: PREFACE Phase transformations occur in most types of materials, including ceramics, metals, polymers, diverse organic and inorganic compounds, minerals, and even crystalline viruses. They have been studied in almost all branches of science, but particularly in physics, chemistry, engineering, materials science and earth sciences. In some cases the objective has been to produce materials in which phase transformations are suppressed, to preserve the structural integrity of some engineering product, for example, while in other cases the objective is to maximise the effects of a transformation, so as to enhance properties such as superconductivity, for example. A long tradition of studying transformation processes in minerals has evolved from the need to understand the physical and thermodynamic properties of minerals in the bulk earth and in the natural environment at its surface. The processes of interest have included magnetism, ferroelasticity, ferroelectricity, atomic ordering, radiation damage, polymorphism, amorphisation and many others—in fact there are very few minerals which show no influence of transformation processes in the critical range of pressures and temperatures relevant to the earth. As in all other areas of science, an intense effort has been made to turn qualitative under-standing into quantitative description and prediction via the simultaneous development of theory, experiments and simulations. In the last few years rather fast progress has been made in this context, largely through an inter-disciplinary effort, and it seemed to us to be timely to produce a review volume for the benefit of the wider scientific community which summarises the current state of the art. The selection of transformation processes covered here is by no means comprehensive, but represents a coherent view of some of the most important processes which occur specifically in minerals. A number of the contributors have been involved in a European Union funded research network with the same theme, under the Training and Mobility of Researchers programme, which has stimulated much of the most recent progress in some of the areas covered. This support is gratefully acknowledged.

Description / Table of Contents: The first half-century of X-ray crystallography, beginning with the elucidation of the sodium chloride structure in 1914, was devoted principally to the determination of increasingly complex atomic topologies at ambient conditions. The pioneering work of the Braggs, Pauling, Wyckoff, Zachariasen and many other investigators revealed the structural details and underlying crystal chemical principles for most rock-forming minerals (see, for example, Crystallography in North America, edited by D. McLachlan and J. P. Glusker, NY, American Crystallographic Association, 1983). These studies laid the crystallographic foundation for modem mineralogy. The past three decades have seen a dramatic expansion of this traditional crystallographic role to the study of the relatively subtle variations of crystal structure as a function of temperature, pressure, or composition. Special sessions on "High temperature crystal chemistry" were first held at the Spring Meeting of the American Geophysical Union (April 19, 1972) and the Ninth International Congress of Crystallography (August 30, 1972). The Mineralogical Society of America subsequently published a special 11-paper section of American Mineralogist entitled "High Temperature Crystal Chemistry," which appeared as Volume 58, Numbers 5 and 6, Part I in July-August, 1973. The first complete three-dimensional structure refinements of minerals at high pressure were completed in the same year on calcite (Merrill and Bassett, Acta Crystallographica B31, 343-349, 1975) and on gillespite (Hazen and Burnham, American Mineralogist 59, 1166-1176, 1974). Rapid advances in the field of non-ambient crystallography prompted Hazen and Finger to prepare the monograph Comparative Crystal Chemistry: Temperature, Pressure, Composition and the Variation of Crystal Structure (New York: Wiley, 1982). At the time, only about 50 publications documenting the three-dimensional variation of crystal structures at high temperature or pressure had been published, though general crystal chemical trends were beginning to emerge. That work, though increasingly out of date, remained in print until recently as the only comprehensive overview of experimental techniques, data analysis, and results for this crystallographic sub-discipline. This Reviews in Mineralogy and Geochemistry volume was conceived as an updated version of Comparative Crystal Chemistry. A preliminary chapter outline was drafted at the Fall 1998 American Geophysical Union meeting in San Francisco by Ross Angel, Robert Downs, Larry Finger, Robert Hazen, Charles Prewitt and Nancy Ross. In a sense, this volume was seen as a "changing of the guard" in the study of crystal structures at high temperature and pressure. Larry Finger retired from the Geophysical Laboratory in July, 1999, at which time Robert Hazen had shifted his research focus to mineral-mediated organic synthesis. Many other scientists, including most of the authors in this volume, are now advancing the field by expanding the available range of temperature and pressure, increasing the precision and accuracy of structural refinements at non-ambient conditions, and studying ever more complex structures. The principal objective of this volume is to serve as a comprehensive introduction to the field of high-temperature and high-pressure crystal chemistry, both as a guide to the dramatically improved techniques and as a summary of the voluminous crystal chemical literature on minerals at high temperature and pressure. The book is largely tutorial in style and presentation, though a basic knowledge of X-ray crystallographic techniques and crystal chemical principles is assumed. The book is divided into three parts. Part I introduces crystal chemical considerations of special relevance to non-ambient crystallographic studies. Chapter 1 treats systematic trends in the variation of structural parameters, including bond distances, cation coordination, and order-disorder with temperature and pressure, while Chapter 2 considers P-V-T equation-of-state formulations relevant to x-ray structure data. Chapter 3 reviews the variation of thermal displacement parameters with temperature and pressure. Chapter 4 describes a method for producing revealing movies of structural variations with pressure, temperature or composition, and features a series of "flip-book" animations. These animations and other structural movies are also available as a supplement to this volume on the Mineralogical Society of America web site at (http://www.minsocam.orgIMSAlRimlRim41.html). Part II reviews the temperature- and pressure-variation of structures in major mineral groups. Chapter 5 presents crystal chemical systematics of high-pressure silicate structures with six-coordinated silicon. Subsequent chapters highlight temperature- and pressure variations of dense oxides (Chapter 6), orthosilicates (Chapter 7), pyroxenes and other chain silicates (Chapter 8), framework and other rigid-mode structures (Chapter 9), and carbonates (Chapter 10). Finally, the variation of hydrous phases and hydrogen bonding are reviewed in Chapter 11, while molecular solids are summarized in Chapter 12. Part III presents experimental techniques for high-temperature and high-pressure studies of single crystals (Chapters 13 and 14, respectively) and polycrystalline samples (Chapter 15). Special considerations relating to diffractometry on samples at non-ambient conditions are treated in Chapter 16. Tables in these chapters list sources for relevant hardware, including commercially available furnaces and diamond-anvil cells. Crystallographic software packages, including diffractometer operating systems, have been placed on the Mineralogical Society web site for this volume. This volume is not exhaustive and opportunities exist for additional publications that review and summarize research on other mineral groups. A significant literature on the high-temperature and high-pressure structural variation of sulfides, for example, is not covered here. Also missing from this compilation are references to a variety of studies of halides, layered oxide superconductors, metal alloys, and a number of unusual silicate structures.

Description / Table of Contents: Since the dawn of life on earth, organisms have played roles in mineral formation in processes broadly known as biomineralization. This biologically-mediated organization of aqueous ions into amorphous and crystalline materials results in materials that are as simple as adventitious precipitates or as complex as exquisitely fabricated structures that meet specialized functionalities. The purpose of this volume of Reviews in Mineralogy and Geochemistry is to provide students and professionals in the earth sciences with a review that focuses upon the various processes by which organisms direct the formation of minerals. Our framework of examining biominerals from the viewpoints of major mineralization strategies distinguishes this volume from most previous reviews. The review begins by introducing the reader to over-arching principles that are needed to investigate biomineralization phenomena and shows the current state of knowledge regarding the major approaches to mineralization that organisms have developed over the course of Earth history. By exploring the complexities that underlie the "synthesis" of biogenic materials, and therefore the basis for how compositions and structures of biominerals are mediated (or not), we believe this volume will be instrumental in propelling studies of biomineralization to a new level of research questions that are grounded in an understanding of the underlying biological phenomena.

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: Many faults appears to form persistent zones of weakness that fundamentally influence the distribution, arichitecture and movement patterns of crustal-scale deformation and associated processes in both continental and oceanic regions. They act as conduits for the focused migration of economically important fluids and, as most seismicity is associated with active faults, they also constitute one of the most important global geological hazards. This book brings together papers by an international group of Earth Scientists to discuss a broad range of topics centred upon the controls of fault weakening and the role of such faults during lithosphere deformation. The book will be of interests to both academic and industrial Earth Scientists with an interest in geodynamics, structure at all scales, tectonics and the migration of petroleum and water.

Description / Table of Contents: As a result of its relative buoyancy, continental crust is rarely subducted, meaning that successive episodes of continental deformation impart a complex geological character that is not found in younger oceanic lithosphere. This character is largely the result of two related processes: (1) reactivation, involving rejuvenation of discrete structures; and (2) reworking, involving the repeated metamorphism, deformation and magmatism of a previously tectonized crustal or lithospheric volume. Characterizing the style, distribution and timing of reactivation and reworking in different continental settings should therefore provide a crucial data set with which to evaluate the spatial patterns, temporal evolution and dynamic controls of tectonic rejuvenation of the continents and continental lithosphere. This volume presents a combination of review and research papers, which highlight some of the issues and problems associated with the characterization and modelling of continental reactivation and reworking.

Description / Table of Contents: Our understanding of rock forming geological processes and thereby of geodynamic processes depends largely on a sound basis of knowledge of minerals. Due to the application of new analytical techniques, the number of newly discovered minerals increases steadily, and what used to be a simple mineral may have turned into a complex group. A continuous update is necessary, and the Reviews in Mineralogy and Geochemistry series excellently fulfills this requirement. The epidote minerals have not yet been covered and we felt that this gap should be filled. The epidote mineral group consists of important rock-forming minerals such as clinozoisite and epidote, geochemical important accessory minerals such as allanite, and minerals typical for rare bulk compositions such as hancockite. Zoisite, the orthorhombic polymorph of clinozoisite, is included here because of its strong structural and paragenetic similarity to the epidote minerals. Epidote minerals occur in a wide variety of rocks, from near-surface conditions up to high- and ultrahigh-pressure metamorphic rocks and as liquidus phases in magmatic systems. They can be regarded as the low-temperature and high-pressure equivalent of Ca-rich plagioclase, and thus are equally important as this feldspar for petrogenetic purposes. In addition, they belong to the most important Fe3+ bearing minerals, and give important information about the oxygen fugacity and the oxidation state of a rock. Last but not least, they can incorporate geochemically relevant minor and trace elements such as Sr, Pb, REE, V, and Mn. The epidote minerals are undoubtedly very important from a petrogenetic and geochemical point of view, and have received a lot of attention in the last years from several working groups in the field of experimental studies and spectroscopic work. As a result, the thermodynamic database of epidote minerals has been significantly enlarged during the last decade. Recent studies have revealed the importance of zoisite in subduction zone processes as a carrier of H2O and suggested zoisite to be the main H2O source in the pressure interval between about 2.0 and 3.0 GPa. Many studies have shown that an understanding of trace element geochemical processes in high-pressure rocks is impossible without understanding the geochemical influence of the epidote minerals. Recent advances in microanalytical techniques have also shown that epidote minerals record detailed information on their geological environment. W. A. Deer, R. A. Howie and J. Zussmann edited the last comprehensive review on this mineral group almost 20 years ago in 1986. In 1990, on the occasion of the 125th anniversary of the discovery of the famous Knappenwand locality in the Tauern/Austria, an epidote conference was held in Neukirchen/Austria organized by the Austrian Mineralogical Society by V. Höck and F. Koller. In 1999, there was a special symposium at the EUG 10 in Strasbourg, convened by R. Gieré and F. Oberli, entitled Recent advances in studies of the epidote group that highlighted the relevance of the epidote minerals for Earth science. However, there are many open questions in the community regarding the epidote minerals and there is a need for a new overview that brings together the recent knowledge on this interesting group of minerals. The present volume of the Reviews in Mineralogy and Geochemistry reviews the current state of knowledge on the epidote minerals with special emphasis on the advances that were made since the comprehensive review of Deer et al. (1986). We hope that it will serve to outline the open questions and direction of future research. In the Introduction, we review the structure, optical data and crystal chemistry of this mineral group, all of which form the basis for understanding much of the following material in the volume. In addition, we provide some information on special topics, such as morphology and growth, deformation behavior, and gemology. Thermodynamic properties (Chapter 2, Gottschalk), the spectroscopy of the epidote minerals (Chapter 3, Liebscher) and a review of the experimental studies (Chapter 4, Poli and Schmidt) constitute the first section of chapters. These fields are closely related, and all three chapters show the significant progress over the last years, but that some of the critical questions such as the problem of miscibility and miscibility gaps are still not completely solved. This section concludes with a review of fluid inclusion studies (Chapter 5, Klemd), a topic that turned out to be of large interest for petrogenetic interpretation, and leads to the description of natural epidote occurrences in the second section of the book. These following chapters review the geological environments of the epdiote minerals, from low temperature in geothermal fields (Chapter 6, Bird and Spieler), to common metamorphic rocks (Chapter 7, Grapes and Hoskin) and to high- and ultrahigh pressure (Chapter 8, Enami, Liou and Mattinson) and the magmatic regime (Chapter 9, Schmidt and Poli). Allanite (Chapter 10, Gieré and Sorensen) and piemontite (Chapter 11, Bonazzi and Menchetti), on which a large amount of information is now available, are reviewed in separate chapters. Finally trace element (Chapter 12, Frei, Liebscher, Franz and Dulski) and isotopic studies, both stable and radiogenic isotopes (Chapter 13, Morrison) are considered. We found it unavoidable that there is some overlap between individual chapters. This is an inherited problem in a mineral group such as the epidote minerals, which forms intensive solid solutions between the major components of rock forming minerals as well as with trace elements.

Description / Table of Contents: The recent surge in energy prices has drawn attention to the availability and security of energy resources, and the prospects for both supply and prices. This book contains a detailed analysis of the trends in global energy production and supply, with the focus on primary energy. It considers the main factors driving energy production and distribution, including: the cost of developing resources and bringing them to market; energy pricing; and the impact of government policies. The study's central finding is that reserves of oil, gas, coal and uranium are more than adequate to meet projected demand growth at least until 2020. However, massive investment in energy production and transportation infrastructure will be needed to exploit these reserves. Beyond 2020, new technologies such as hydrogen-based fuel cells, clean coal burning and carbon sequestration hold out the prospect of abundant and clean energy supplies in a world largely free of climate-destabilising carbon emissions.

Description / Table of Contents: PREFACE Sulfate is an abundant and ubiquitous component of Earth’s lithosphere and hydrosphere. Sulfate minerals represent an important component of our mineral economy, the pollution problems in our air and water, the technology for alleviating pollution, and the natural processes that affect the land we utilize. Vast quantities of gypsum are consumed in the manufacture of wallboard, and calcium sulfates are also used in sculpture in the forms of alabaster (gypsum) and papier-mâché (bassanite). For centuries, Al-sulfate minerals, or “alums,” have been used in the tanning and dyeing industries, and these sulfate minerals have also been a minor source of aluminum metal. Barite is used extensively in the petroleum industry as a weighting agent during drilling, and celestine (also known as “celestite”) is a primary source of strontium for the ceramics, metallurgical, glass, and television face-plate industries. Jarosite is a major waste product of the hydrometallurgical processing of zinc ores and is used in agriculture to reduce alkalinity in soils. At many mining sites, the extraction and processing of coal or metal-sulfide ores (largely for gold, silver, copper, lead, and zinc) produce waste materials that generate acid-sulfate waters rich in heavy metals, commonly leading to contamination of water and sediment. Concentrated waters associated with mine wastes may precipitate a variety of metal-sulfate minerals upon evaporation, oxidation, or neutralization. Some of these sulfate minerals are soluble and store metals and acidity only temporarily, whereas others are insoluble and improve water quality by removing metals from the water column. There is considerable scientific interest in the mineralogy and geochemistry of sulfate minerals in both high-temperature (igneous and hydrothermal) and low-temperature (weathering and evaporite) environments. The physical scale of processes affected by aqueous sulfate and associated minerals spans from submicroscopic reactions at mineral-water interfaces to global issues of oceanic cycling and mass balance, and even to extraterrestrial applications in the exploration of other planets and their satellites. In mineral exploration, minerals of the alunite-jarosite supergroup are recognized as key components of the advanced argillic (acid-sulfate) hydrothermal alteration assemblage, and supergene sulfate minerals can be useful guides to primary sulfide deposits. The role of soluble sulfate minerals formed from acid mine drainage (and its natural equivalent, acid rock drainage) in the storage and release of potentially toxic metals associated with wet-dry climatic cycles (on annual or other time scales) is increasingly appreciated in environmental studies of mineral deposits and of waste materials from mining and mineral processing. This volume compiles and synthesizes current information on sulfate minerals from a variety of perspectives, including crystallography, geochemical properties, geological environments of formation, thermodynamic stability relations, kinetics of formation and dissolution, and environmental aspects. The first two chapters cover crystallography (Chapter 1) and spectroscopy (Chapter 2). Environments with alkali and alkaline earth sulfates are described in the next three chapters, on evaporites (Chapter 3). barite-celestine deposits (Chapter 4), and the kinetics of precipitation and dissolution of gypsum, barite, and celestine (Chapter 5). Acidic environments are the theme for the next four chapters, which cover soluble metal salts from sulfide oxidation (Chapter 6), iron and aluminum hydroxysulfates (Chapter 7), jarosites in hydrometallugy (Chapter 8), and alunite-jarosite crystallography, thermodynamics, and geochronology (Chapter 9). The next two chapters discuss thermodynamic modeling of sulfate systems from the perspectives of predicting sulfate-mineral solubilities in waters covering a wide range in composition and concentration (Chapter 10) and predicting interactions between sulfate solid solutions and aqueous solutions (Chapter 11). The concluding chapter on stable-isotope systematics (Chapter 12) discusses the utility of sulfate minerals in understanding the geological and geochemical processes in both high-and low-temperature environments, and in unraveling the past evolution of natural systems through paleoclimate studies. We thank the authors for their comprehensive and timely efforts, and for their cooperation with our various requests regarding consistency of format and nomenclature. Special thanks are due to the numerous scientists who provided peer reviews, which substantially improved the content of the chapters. This volume would not have been possible without the usual magic touch and extreme patience of Paul H. Ribbe, Series Editor for Reviews in Mineralogy and Geochemistry. Finally, we thank our families for their support and understanding during the past several months.

Description / Table of Contents: Vol. 157, 2000 spanning across disciplines and national boundaries gives cause for optimism. New participation in ACES to extend its existing synergies is welcomed. We wish to thank the scientific participants of The APEC Cooperation for Earthquake Simulation (ACES) and the contributors to this book. We express appreciation to the Australian, Chinese, Japanese and USA governments for supporting the establishment of ACES. We gratefully acknowledge funding support by the Australian government's Department of Industry, Science and Resources, The University of Queensland, Japan's Science and Technology Agency through its Research Organisation for Information Science and Technology, the Chinese Ministry of Science and Technology, and the National Science Foundation of China. We acknowledge with appreciation additional workshop sponsorship pro­ vided by SGI (Silicon Graphics). Special thanks to QUAKES team members (Tracy Paroz, David Place, Steffen Abe, Dion Weatherley and Steven Jaume) and Kim Olsen who provided assistance to the Editors. Peter Mora would also like to thank Evelyne Meier. REFERENCES I-st ACES Workshop Proceedings (1999), ed. Mora, P. (ACES, Brisbane, Australia, ISBN 1 86499 121 6), 554 pp. APEC Cooperation for Earthquake Simulation: http://quakes. earth. uq. edu. au/ACES ACES Inaugural Workshop: http://quakes. earth. uq. edu. au/ACES_ WS Raul Madariaga Peter Mora QUAKES Laboratoire de Geologie Department of Earth Sciences Ecole Normale Superieur The University of Queensland 24 Rue Lhomond 4072 Brisbane, Qld F-75231 Paris, Cedex 05 Australia France mora@earth. up. edu. au madariag@geologie. ens.

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: 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: 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: 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: "Maxwell is without peer. This printing is an opportunity to become thoroughly acquainted with the thought of the greatest of our electrical scientists." — School Science and MathHere is the final elaboration of Maxwell's theory of electromagnetism, including the systematic and rigorous derivation of his general equations of field theory. These equations continue to occupy a central position in the modern physicist's view of the physical world. They are a magnificent summary of the fundamental advances in electricity and magnetism, and later inspired the theories of Lorentz on the electron and Einstein on relativity. Einstein himself has said that "The formulation of these equations is the most important event in physics since Newton's time." (The Evolution of Physics.) Volume 1, Part 1, "Electrostatics," describes electrostatic phenomena and develops a mathematical theory of electricity. Maxwell discusses electrical work and energy in a system of conductors, mechanical action between two electrical systems, forms of equipotential surfaces and line of flow, spherical harmonics, the theory of electric images, and other topics. Part II, "Electrokinematics," deals with electric current conduction and resistance, electromotive force between bodies in contact, electrolysis, the mathematical theory of the distribution of electric currents, and other topics.

Description / Table of Contents: Prof. Dr. -Ing. Wolfgang Spyra Brandenburg University of Technology in Cottbus, Germany The demilitarization and conversion of military properties wor- wide has been a topic of growing importance since the end of the Cold War. The slowing of the arms race brought on by weapons treaties and relaxed tensions between NATO and Warsaw Pact nations caused sto- piles of conventional weapons to become superfluous. The need to process and dispose of such weapons began more quickly in NATO countries. This demilitarization process began shortly after the reunification of Germany and was largely completed by the mid to late 1990’s. The remaining process, no small task in itself, of converting lands formerly used by the military into safe and environmentally acceptable landscapes may continue for decades to come. Due to a lack of resources and technology, the process of demilitarization in the former Warsaw Pact countries has launched more slowly. In 2002 both Georgia and Moldova finished projects which destroyed their stocks of liquid ballistic missile components. Both these projects were carried out through the cooperative support of trans-national organizations, private contractors, and research institutions. The Republic of Azerbaijan now finds itself at the beginning of its demilitarization process. Stored at the country’s military depots are over 2000 tons of missile fuels, oxidizer, and chemical additives. This hazardous waste is kept in tanks intended only for temporary transport and storage.

Description / Table of Contents: Synthetic Discussions --- Geophysical Studies of the Northern Cascadia Subduction Zone off Western Canada and Their Implications for Great Earthquake Seismotectonics: A Review / Ron M. Clowes and Roy D. Hyndman / pp. 1-23 --- Understanding the Seismotectonics of the Cascadia Subduction Zone: Overview and Recent Seismic Work / Thomas L. Pratt, Craig S. Weaver, Thomas M. Brocher, Thomas Parsons, Michael A. Fisher, Kenneth C. Creager, Robert S. Crosson, Roy D. Hyndman, George Spence, Anne M. Tréhu, Kate C. Miller and Uri S. TEN Brink / pp. 25-36 --- Long-Term Probabilistic Forecast in Japan and Time-Predictable Behavior of Earthquake Recurrence / Kunihiko Shimazaki / pp. 37-43 --- Recipe for Estimating Strong Ground Motions from Active Fault Earthquakes / Kojiro Irikura / pp. 45-55 --- Seismic Velocity --- New Features of Island Arc Crust Inferred from Seismic Refraction/Wide-Angle Reflection Expeditions in Japan / Takaya Iwasaki, Toshikatsu Yoshii, Naoshi Hirata and Hiroshi Sato / pp. 57-70 --- Seeking the Cause of Large Crustal Earthquakes in Japan: Influence of Arc Magma and Fluids / Dapeng Zhao / pp. 71-91 --- Conductivity --- Stress, Stress Release and Geoelectromagnetism / Fiona Simpson / pp. 93-106 --- Network-MT Survey in Japan to Determine Nation-Wide Deep Electrical Conductivity Structure / Makoto Uyeshima, Masahiro Ichiki, Ikuko Fujii, Hisashi Utada, Yasunori Nishida, Hideyuki Satoh, Masaaki Mishina, Tadashi Nishitani, Satoru Yamaguchi, Ichiro Shiozaki, Hideki Murakami and Naoto Oshiman / pp. 107-121 --- Understanding of Seismic Activity Using Conductivity Data in the Central Part of Northeastern Japan / Yukio Fujinawa, Noriaki Kawakami, Jun Inoue, Theodore H. Asch, Shinji Takasugi and Yoshimori Honkura / pp. 123-140 --- Crustal Activity --- Monitoring of Crustal Deformation in Japan Using L-band SAR Interferometry / Makoto Murakami, Satoshi Fujiwara, Takuya Nishimura, Mikio Tobita, Hiroyuki Nakagawa, Shinzaburo Ozawa and Masaki Murakami / pp. 141-146 --- Detection of a Coupling State in the Tokai Plate-Subducting Region Based on Microearthquake Seismicity and on Crustal Deformation / Shozo Matsumura / pp. 147-155 --- Coseismic Slip Distribution of the 1944 Tonankai and 1946 Nankai Earthquakes / Yuichiro Tanioka / pp. 157-165 --- The Southern California Integrated GPS Network (SCIGN) / Kenneth W, Hudnut, Yehuda Bock, John E. Galetzka, Frank H. Webb and William H. Young / pp. 167-189 --- Crustal Movement in Southwest Japan, Deduced from Continuous GPS Measurements, and Its Seismotectonic Implications / Kaoru Miyashita, Jianxin Li and Takashi Kawachi / pp. 191-200 --- Active Faults --- Deep Geometry and Evolution of Active Faults in Northern Honshu, Japan / Hiroshi Sato, Naoshi Hirata And Takaya Iwasaki / pp. 201-207 --- Rupturing History of Active Faults during the Last 1000 Years in the Central Japan / Eikichi Tsukuda / pp. 209-218 --- Active Faulting, Lower Crustal Delamination and Ongoing Hidaka Arc-Arc Collision, Hokkaido, Japan / Tanio Ito / pp. 219-224 --- Seismotectonics in the Subduction Zone: Japan --- Inhomogeneous Structure of the Crust and Its Relationship to Earthquake Occurrence / Norihito Umino and Akira Hasegawa / pp. 225-235 --- Configuration of the Philippine Sea Slab and Seismic Activity in the Tokai Region, Central Japan / Satoshi Harada and Akio Yoshida / pp. 237-246 --- On-Line Operating Network of the High Gain Seismometers and Tsunami Sensors, Deployed at the Sea-Floor of the Sagami Trough Subduction Zone, Central Japan / Takao Eguchi, Yukio Fujinawa, Eisuke Fujita, Sin-Iti Iwasaki, Isao Watabe, Hiroaki Negishi and Hiroyuki Fujiwara / pp. 247-260 --- Seismotectonics around the Active Convergent Zones --- Seismotectonics of the Frontal Himalaya through the Electrical Conductivity Imaging / B. R. Arora / pp. 261-272 --- Models of Subduction Zones --- A Simple Review on the Simulation of Earthquake Cycle at Subduction Zones / Kazuro Hirahara / pp. 273-282 --- Systematic Variations in Non-Local Seismicity Patterns in Southern California / K. F. Tiampo, J. B. Rundle, S. McGinnis, W. Klein and S. J. Gross / pp. 283-292 --- Earthquake in Turkey --- Deep Resistivity Structure around the Fault Associated with the 1999 Kocaeli Earthquake, Turkey / N. Oshiman, R. Yoshimura, T. Kasaya, Y. Honkura, M. Matsushima, S. Baris, C. Celik, M. K. Tuncer and A. M. Isikara / pp. 293-303 --- S Wave Splitting Observation inside of the North Anatolian Fault, Turkey / Keiichi Tadokoro, Masataka Ando, Serif Baris, Kin'ya Nishigami, Mamoru Nakamura, S. Balamir Ücer, Akihiko Ito, Yoshimori Honkura and A. Mete Isikara / pp. 305-310 --- Earthquake in Taiwan --- Drilling the Chelungpu Fault, Taiwan: Cores and Heat-Flow from a Thrust-Fault with Very Large Displacements in a Recent Earthquake / Masataka Ando, James Mori, Hidemi Tanaka and Kuo-Fong Ma / pp. 311-317 --- The Ms7.6 Chi-Chi, Taiwan, Earthquake of September 20, 1999 / J.-H. Wang, R.-D. Hwang, B.-S. Huang, K.-C. Chen, W.-G. Huang, and T.-M. Chang / pp. 319-324 --- Some Observations about the Chi-Chi, Taiwan Earthquake of September 21, 1999 / Yi-Ben Tsai / pp. 325-366 --- In-situ Measurements to Understand Seismotectonics in the Subduction Zone --- Borehole Observatories into Subduction Seismogenic Zones / Kiyoshi Suyehiro / pp. 367-374 --- Continental Scientific Drilling for Studying Plate Subduction Earthquakes / Ryuji Ikeda / pp. 375-382 --- Scismotectonics Applied to Earthquake Hazard Mitigation --- Stress Drop Distribution of Micro-Earthquakes at Ootaki, Nagano Prefecture, Japan, Obtained from Waveform Data by Borehole Stations / Shigeki Horiuchi and Yoshihisa Iio / pp. 383-391 --- Site Amplification of' K-NET Sites in the Kanto Region, Central Japan / Shigeo Kinoshita and Yousuke Ogue / pp. 393-405 --- Caltech-USGS Element of TriNet: Remote Stations, Communications, and Data Acquisition / E. Hauksson, P. Maechling, R. Busby and H. Kanamori / pp. 407-423 --- Microzoning Studies for Seismic Risk Mitigation / Kazuoh Seo, Diana Polonska, Katsumi Kurita and Kentaro Motoki / pp. 425-450 --- Earthquake Clusters in the Kanto and Tokai Subduction Zones: Implications for Modes of Plate Consumption / Shin-ichi Noguchi / pp. 451-467 --- Seismic Scattering from Small-Scale Heterogeneities: Numerical Simulations and Observation / Kiyoshi Yomogida / pp. 469-480 --- Tectonic Characteristics of Seismogenic Stress Field in East Asia / Jiren Xu, Zhixin Zhao and Kazuo Oike / pp. 481-497

Description / Table of Contents: A New Outlook and New Resources / pp. 1-7 --- Ocean Water and Its Wonderful Potential / pp. 9-30 --- OTEC Is Not a Dream / pp. 31-44 --- Sea-Water Rears Fish / pp. 45-81 --- Learning from the Past / pp. 83-90 --- Earth-Friendly Technology / pp. 91-94

Description / Table of Contents: MARINE CARBON CYCLE --- Global Scale --- Characterization of Ocean Productivity Using a New Physical-Biological Coupled Ocean Model / K. Nakata, T. Doi, K. Taguchi and S. Aoki / Global Environmental Change in the Ocean and on Land, / pp. 1-44 --- Natural Radiocarbon Distribution in the Deep Ocean / K. Matsumoto and R. M. Key / Global Environmental Change in the Ocean and on Land, / pp. 45-58 --- Equatorial Region --- Variability of Surface Layer CO2 Parameters in the Western and Central Equatorial Pacific / M. Ishii, S. Saito, T. Tokieda, T. Kawano, K. Matsumoto and H. Y. Inoue / Global Environmental Change in the Ocean and on Land, / pp. 59-94 --- Settling Particles Flux in Response to El Niño/Southern Oscillation (ENSO) in the Equatorial Pacific / H. Kawahata and L. P. Gupta / Global Environmental Change in the Ocean and on Land, / pp. 95-108 --- Particulate Amino Acids and Biogeochemical Processes in the Equatorial Pacific Ocean during the 1999-2001 La Niña Event / L. P. Gupta and H. Kawahata / Global Environmental Change in the Ocean and on Land, / pp. 109-120 --- Floral Response of Coccolithophores to Progressive Oligotrophication in the South Equatorial Current, Pacific Ocean / K. Hagino and H. Okada / Global Environmental Change in the Ocean and on Land, / pp. 121-132 --- Coccolith Carbonate Fluxes in the Northwest Pacific Ocean / Y. Tanaka / Global Environmental Change in the Ocean and on Land, / pp. 133-146 --- Western Pacfic --- Artificial Radionuclides in the Western North Pacific: A Review / G. H. Hong, M. Baskaran and P. P. Povinec / Global Environmental Change in the Ocean and on Land, / pp. 147-172 --- Material Transport Processes on the Continental Margin in the East China Sea / M. Yamada / Global Environmental Change in the Ocean and on Land, / pp. 173-187 --- Cadmium Distribution in the Western Pacific / K. Abe / Global Environmental Change in the Ocean and on Land, / pp. 189-203 --- Ocean Environments in Response to Climatic Change --- Climate Reconstructions from Annually Banded Corals / T. Felis and J. Pätzold / Global Environmental Change in the Ocean and on Land, / pp. 205-227 --- Reef Water CO2 System and Carbon Production of Coral Reefs: Topographic Control of System-Level Performance / A. Suzuki and H. Kawahata / Global Environmental Change in the Ocean and on Land, / pp. 229-248 --- Chemistry of Benthic Foraminiferal Shells for Recording Ocean Environments: Cd/Ca, d13C and Mg/Ca / K. Tachikawa and H. Elderfield / Global Environmental Change in the Ocean and on Land, / pp. 249-263 --- Have the Tropical Pacific Ocean-Atmosphere Interactions Behaved as a Driver of Centennial- to Orbital-Scale Climate Changes? / M. Yamamoto / Global Environmental Change in the Ocean and on Land, / pp. 265-278 --- Long Term Variations of Uranium Isotopes and Radiocarbon in the Surface Seawater Recorded in Corals / Y. Yokoyama and T. M. Esat / Global Environmental Change in the Ocean and on Land, / pp. 279-309 --- TERRESTRIAL CARBON CYCLE --- A Multi-Scale Analysis of a National Terrestrial Carbon Budget and the Effects of Land-Use Change / C. M. Trotter, K. R. Tate, S. Saggar, N. A. Scott and M. A. Sutherland / Global Environmental Change in the Ocean and on Land, / pp. 311-341 --- Global Mapping of Terrestrial Primary Productivity and Light-Use Efficiency with a Process-Based Model / A. Ito and T. Oikawa / Global Environmental Change in the Ocean and on Land, / pp. 343-358 --- Carbon and Nitrogen Accumulation in a Savanna Landscape: Field and Modeling Perspectives / S. Archer, T. W. Boutton and C. R. McMurtry / Global Environmental Change in the Ocean and on Land, / pp. 359-373 --- Estimating Dynamics of CO2 Flux in Agro-Ecosystems based on Synergy of Remote Sensing and Process Modeling-A Methodological Study / Y. Inoue and A. Olioso / Global Environmental Change in the Ocean and on Land, / pp. 375-390 --- Changes in Productivity of East and South Asian Countries in the 21st Century: Regional Trends According to Climate Change / K. Okamoto, M. Yokozawa and H. Kawashima / Global Environmental Change in the Ocean and on Land, / pp. 391-399 --- A Preliminary Study on the Carbon Dynamics of China's Forest Ecosystems in the Past 20 Years / P. Gong, J. Chen and M. Xu / Global Environmental Change in the Ocean and on Land, / pp. 401-410 --- Retrieval of Forest Fire History in Far East Asia by Remote Sensing and Its Analysis with Biomass Burning Simulation and Climate Anomalies / J. Kuçera and Y. Yasuoka / Global Environmental Change in the Ocean and on Land, / pp. 411-424 --- Potential of Woody Carbon Stock Estimation Using High Spatial Resolution Imagery: A Case Study of Spruce Stands / Y. Awaya, S. Tsuyuki, E. Kodani and G. Takao / Global Environmental Change in the Ocean and on Land, / pp. 425-440 --- Multi-Temporal MODIS Data Product for Carbon Cycles Research / Z. Dafang, L. Ronggao and S. Runhe / Global Environmental Change in the Ocean and on Land, / pp. 441-451 --- Photosynthetic Characteristics of Mixed Deciduous-Broadleaf Forests from Leaf to Stand / T. Koike, S. Kitaoka, T. Ichie, T. T. Lei and M. Kitao / Global Environmental Change in the Ocean and on Land, / pp. 453-472 --- Effect of Free-Air CO2 Enrichment on Structures of Weed Communities and CO2 Exchange at the Flood-Water Surface in a Rice Paddy Field / H. Koizumi, T. Kibe, T. Nakadai, Y. Yazaki, M. Adachi, M. Inatomi, M. Kondo and T. Ohtsuka / Global Environmental Change in the Ocean and on Land, / pp. 473-485

Description / Table of Contents: Session 1. Global Warming Prediction—Current Status and Issues --- Global Warming Projection Studies at the Meteorological Research Institute/JMA / T. Tokioka and A. Noda / pp. 1-14 --- Projections of Future Climate Change in the 21st Century Simulated by the CCSR/NIES CGCM under the IPCC SRES Scenarios / T. Nozawa, S. Emori, A. Numaguti, Y. Tsushima, T. Takemura, T. Nakajima, A. Abe-Ouchi and M. Kimoto / pp. 15-28 --- Session 2. Modeling of the Atmosphere and Oceans --- Toward a Unified Highly Resolved Regional Climate Modeling System / Y. Wang and B. Wang / pp. 29-48 --- Studies of Climate Variability Using General Circulation Models / M. Kimoto / pp. 49-62 --- Session 3. Modeling of Chemistry of the Atmosphere --- Tropospheric Ozone and Climate: Past, Present and Future / G. P. Brasseur, J.-F. Müller, X-X. Tie and L. Horowitz / pp. 63-76 --- Effects of Man-Made Air Pollution on the Climate / T. Nakajima, A. Higurashi, K. Kawamoto and T. Takemura / pp. 77-88 --- Tropospheric Chemical Transport Modeling over East Asia / I. Uno / pp. 89-100 --- Session 4. Modeling of Land Hydrology Including Snow and Ice --- Effects of Soil Moisture of the Asian Continent upon the Baiu Front / F. Kimura and T. Yoshikane / pp. 101-110 --- Macroscale Hydrology: Challenges and Opportunities / D. P. Lettenmaier / pp. 111-136 --- Linking Ground Hydrology to Ecosystems and Carbon Cycle in a Climate Model / R. E. Dickinson / pp. 137-144 --- Session 5. Modeling of Ecosystem and Its Global Change --- Carbon Storage in the U.S. Caused by Land Use Change / S. W. Pacala, G. C. Hurtt, P. R. Moorcroft and J. P. Caspersen / pp. 145-172 --- A Multi-layered Integrated Numerical Model of Surface Physics—Growing Plants Interaction, MINoSGI / T. Hara, T. Watanabe, M. Yokozawa, S. Emori, K. Takata and A. Sumida / pp. 173-186 --- Session 6. Carbon Cycle Modeling --- Modeling Carbon-Climate Interactions / I. Fung / pp. 187-194 --- Development of Coupled Ocean Physical-Biogeochemical-Ecosystem Model / Y. Yamanaka / pp. 195-206 --- Modeling Carbon Dynamics of Terrestrial Ecosystems in Monsoon Asia / T. Oikawa and A. Ito / pp. 207-220 --- Session 7. Modeling of Paleoenvironmental Change Including Ice Sheet Modeling --- Ice in the Climate System: Paleoclimatological Perspectives / W. R. Peltier and L. P. Solheim / pp. 221-242 --- Using Model Hierarchies to Better Understand Past Climate Chang / M. Kageyama / pp. 243-252 --- Abrupt Climate Change and Thermohaline Circulation / S. Manabe / pp. 253-254 --- Session 8. Modeling of Land Use/Cover Change due to Human Activities --- Backward Land-Cover Change Projections for the Sudano-Sahelian Countries of Africa with a Dynamic Simulation Model of Land-Use Change (SALU) / N. Stephenne and E. F. Lambin / pp. 255-270 --- Integrating Biophysical and Socioeconomic Factors in Modeling Impacts of Global Environmental Change / G. Fischer / pp. 271-292 --- Integration of Observational Data and Behavioral Models for Spatio-Temporal Interpolation—Application to Reconstructing Long-Term Land Use and Land Cover Changes / R. Shibasaki and S. Huang / pp. 293-310 --- Session 9. Integrated Modeling—Current Status --- Earth System Modeling—An Integrated Assessment Tool for Environmental Studies / R. A. Pielke, Sr. / pp. 311-338 --- Integrated Assessment Model of Climate Change: The AIM Approach / Y. Matsuoka, T. Morita and M. Kainuma / pp. 339-362 --- Session 10. Discussion on Strategy toward Modeling of the Integrated System / A. Sumi and T. Morita / pp. 363-372 --- Poster Session --- Effect of Cloud Condensation Nuclei on the Optical Properties of a Layer Cloud: Numerical Simulation with a Cloud-Microphysical Model / N. Kuba, H. Iwabuchi, K. Maruyama, T. Hayasaka and T. Takeda / pp. 373-374 --- Intercontinental Transport and Chemical Transformation of Ozone and Its Precursors from East Asia / O. Wild and H. Akimoto / pp. 375-382 --- Development of CCSR/NIES Nudging CTM and Ozone Simulation / H. Akiyoshi, M. Takigawa, T. Nagashima, J. Kurokawa, S. Sugata, M. Takahashi and H. Nakane / pp. 383-390 --- Modeling Surface Hydrology for Global Water Cycle Simulations / T. Oki / pp. 391-404 --- A New Frozen Soil Parameterization in Land Surface Scheme / X. Li and T. Koike / pp. 405-414 --- Individual-Based Model of a Forest with Spatial Structure and Gene Flow / A. Takenaka / pp. 415-420 --- Global Potential of Carbon Sinks under the Kyoto Protocol / Y. Yamagata and G. A. Alexandrov / pp. 421-426 --- Effect of Orography on Land and Ocean Surface Temperature / A. Kitoh / pp. 427-432 --- Regional Warming Related with Land Use Change during Past 135 Years in Japan / T. Ichinose / pp. 433-440 --- Development of Land Use Model for IPCC New Emission Scenarios (SRES) / T. Masui, Y. Matsuoka, T. Morita, M. Kainuma and K. Takahashi / pp. 441-448 --- Numerical Simulation Study Using a Climate Model Includinga Sophisticated Land Surface Model / K. Mabuchi, Y. Sato and H. Kida / pp. 449-456

Description / Table of Contents: In the last decade of the 20th century, there has been great progress in the physics of earthquake generation; that is, the introduction of laboratory-based fault constitutive laws as a basic equation governing earthquake rupture, quantitative description of tectonic loading driven by plate motion, and a microscopic approach to study fault zone processes. The fault constitutive law plays the role of an interface between microscopic processes in fault zones and macroscopic processes of a fault system, and the plate motion connects diverse crustal activities with mantle dynamics. An ambitious challenge for us is to develop realistic computer simulation models for the complete earthquake process on the basis of microphysics in fault zones and macro-dynamics in the crust-mantle system. Recent advances in high performance computer technology and numerical simulation methodology are bringing this vision within reach. The book consists of two parts and presents a cross-section of cutting-edge research in the field of computational earthquake physics. Part I includes works on microphysics of rupture and fault constitutive laws, and dynamic rupture, wave propagation and strong ground motion. Part II covers earthquake cycles, crustal deformation, plate dynamics, and seismicity change and its physical interpretation. Topics covered in Part I range from the microscopic simulation and laboratory studies of rock fracture and the underlying mechanism for nucleation and catastrophic failure to the development of theoretical models of frictional behaviors of faults; as well as the simulation studies of dynamic rupture processes and seismic wave propagation in a 3-D heterogeneous medium, to the case studies of strong ground motions from the 1999 Chi-Chi earthquake and seismic hazard estimation for Cascadian subduction zone earthquakes.

Description / Table of Contents: This volume, "Air Quality", contains many original findings on biomasss fires, transboundary pollution and associated haze and their impacts on health, biodiversity and economy and thus is expected to be a source book for research in South East Asia. Many of the results presented in this volume pertain to this region and are thus available under one "roof". Some papers could be discussed in graduate level classes dealing with Air Pollution, Air Quality, Cloud Physics and Biophysics. The scientific community will find this book a useful addition to their personal and institutional libraries.

Description / Table of Contents: In the wake of the disastrous tsunami which struck Papua New Guinea in 1998, this volume presents 20 state-of-the-art contributions on landslide tsunamis, including earthquake characteristics and ground motions, modeling of landslides in geotechnical engineering, field surveys on land and at sea, simulations of past, present, and potential future tsunamis, and theoretical studies of tsunami generation by landslides.

Description / Table of Contents: Geophysicists use seismic signals to image structures in the Earth's interior, to understand the mechanics of earthquake and volcanic sources, and to estimate their associated hazards. Keiiti Aki developed pioneering quantitative methods for extracting useful information from various portions of observed seismograms and applied these methods to many problems in the above fields. This volume honors Aki's contributions with review papers and results from recent applications by his former students and scientific associates pertaining to topics spawned by his work. Discussed subjects include analytical and numerical techniques for calculating dynamic rupture and radiated seismic waves, stochastic models used in engineering seismology, earthquake and volcanic source processes, seismic tomography, properties of lithospheric structures, analysis of scattered waves, and more. The volume will be useful to students and professional geophysicists alike.

Description / Table of Contents: Concepts and methods of fractal geometry penetrate various branches of human knowledge to an increasing degree. This tendency is particularly striking in the geosciences, because many processes occurring in and on the Earth result in time dependences and spatial patterns that have a fractal character. The contributions in this volume arose from the "3rd International Symposium on Fractals and Dynamic Systems in Geosciences", held at Stara Lesna, Slovakia in June, 1997. The volume contains new ideas and applications of fractal geometry in such diverse branches of geoscience as engineering geology, the physics of the lithosphere (including faulting, seismicity, and fluid flow), and climate behavior.

Description / Table of Contents: The Azores-Tunisia region is formed by the western part of the plate boundary between Eurasia and Africa. This plate boundary presents a complex nature due to its proximity to the pole of rotation of the African plate. This condition produces crustal extensions and normal faulting at the Azores archipelago, transcurrent motion with strike slip faulting at the center part of the Azores-Gibraltar fault and at the eastern end, from the Gulf of Cadiz to Tunisia, plate convergence with reverse faulting. In this last part, the collision of Iberia with northern Morocco produces complex phenomena with intermediate depth and deep earthquakes and an extensional regime at the Alboran sea. Recently, new evidence has been gathered in this region based on observations from geology, geodesy, mainly through GPS measurements, seismology, especially with the installation of broad-band stations, and other fields of geophysics, such as paleomagnetism and gravimetry.

Description / Table of Contents: The supply and protection of groundwater, the production of hydrocarbon reservoirs, land subsidence in coastal areas, exploitation of geothermal energy, the long-term disposal of critical wastes ... What do these issues have in common besides their high socio-economic impact? They are all closely related to fluid flow in porous and/or fractured rock. As the conditions of fluid flow in many cases depend on the mechanical behavior of rocks, coupling between the liquid phase and the rock matrix can generally not be neglected. For the past five years or so, studies of rock physics and rock mechanics linked to coupling phenomena have received increased attention. In recognition of this, a Euroconference on thermo-hydro-mechanical coupling in fractured rock was held at Bad Honnef, Germany, in November 2000. Most of the twenty papers collected in this volume were presented at this meeting. The contributions lead to deeper insight in processes where such coupling is relevant.

Description / Table of Contents: "Beyond Wavelets" presents state-of-the-art theories, methods, algorithms, and applications of mathematical extensions for classical wavelet analysis. Wavelets, introduced 20 years ago by Morlet and Grossmann and developed very rapidly during the 1980's and 1990's, has created a common link between computational mathematics and other disciplines of science and engineering. Classical wavelets have provided effective and efficient mathematical tools for time-frequency analysis which enhances and replaces the Fourier approach. However, with the current advances in science and technology, there is an immediate need to extend wavelet mathematical tools as well. "Beyond Wavelets" presents a list of ideas and mathematical foundations for such extensions, including: continuous and digital ridgelets, brushlets, steerable wavelet packets, contourlets, eno-wavelets, spline-wavelet frames, and quasi-affine wavelets. Wavelet subband algorithms are extended to pyramidal directional and nonuniform filter banks. In addition, this volume includes a method for tomographic reconstruction using a mechanical image model and a statistical study for independent adaptive signal representation. Investigators already familiar with wavelet methods from areas such as engineering, statistics, and mathematics will benefit by owning this volume. *Curvelets, Contourlets, Ridgelets, *Digital Implementation of Ridgelet Packets *Steerable Wavelet Packets *Essentially Non-Oscillatory Wavelets *Medical Imaging *Non-Uniform Filter Banks *Spline-wavelet frames and *Vanishing Moment Recovery Functions