ALBERT

Description / Table of Contents: Fold-and-thrust belts occur worldwide, have formed in all eras of geological time, and are widely recognized as the most common mode in which the crust accommodates shortening. Much current research on the structure of fold-and-thrust belts is focused on structural studies of regions or individual structures and on the geometry and evolution of these regions employing kinematic, mechanical and experimental modelling. In keeping with the main trends of current research, this title is devoted to the kinematic evolution and structural styles of a number of fold-and-thrust belts formed from Palaeozoic to Recent times. The papers included in this book cover a broad range of different topics, from modelling approaches to predict internal deformation of single structures, 3D reconstructions to decipher the structural evolution of groups of structures, palaeomagnetic studies of portions of fold-and-thrust belts, geometrical and kinematical aspects of Coulomb thrust wedges and structural analyses of fold-and-thrust belts to unravel their sequence of deformations.

Description / Table of Contents: The past decade has witnessed a major revival in attempts to separate biodiversity signals from biases imposed by sampling and the architecture of the rock record. How large a problem this poses to our understanding of biodiversity patterns remains debatable, and new approaches are being developed to investigate this question. Here palaeobiologists with widely differing approaches and interests explore the problems of extracting reliable information on biodiversity change from an imperfect geological record. Topics covered range from the application of information-theoretic approaches that identify directional causal relationships to an in-depth study of how geological biases could influence our understanding of dinosaur evolution. A wide range of new insights into the links between the land, shallow-marine and deep-sea rock and fossil records are presented, making this volume invaluable to anyone in the Earth or life sciences who wishes to remain abreast of this dynamic and rapidly evolving research area.

Description / Table of Contents: This collection of papers presents recent advances in the study of deformation mechanisms and rheology and their applications to tectonics. Many of the contributions exploit new petrofabric techniques, particularly electron backscatter diffraction, to help understand evolution of rock microstructure and mechanical properties. Papers in the first section (lattice preferred orientations and anisotropy) show a growing emphasis on the determination of elastic properties from petrofabrics, from which acoustic properties can be computed for comparison with in-situ seismic measurements. Such research will underpin geodynamic interpretation of large-scale active tectonics. Contributions in the second section (microstructures, mechanisms and rheology) study the relations between microstructural evolution during deformation and mechanical properties. Many of the papers explore how different mechanisms compete and interact to control the evolution of grain size and petrofabrics. Contributors make use of combinations of laboratory experiments, field studies and computational methods, and several relate microstructural and mechanical evolution to large-scale tectonic processes observed in nature.

Description / Table of Contents: Human impact on our environment is not a new phenomenon. For millennia, humans have been coping with – or provoking – environmental change. We have exploited, extracted, over-used, but also in many cases nurtured, the resources that the geosphere offers. Geoarchaeology studies the traces of human interactions with the geosphere and provides the key to recognizing landscape and environmental change, human impacts and the effects of environmental change on human societies. This collection of papers from around the world includes case studies and broader reviews covering the time period since before modern human beings came into existence up until the present day. To understand ourselves, we need to understand that our world is constantly changing, and that change is dynamic and complex. Geoarchaeology provides an inclusive and long-term view of human–geosphere interactions and serves as a valuable aid to those who try to determine sustainable policies for the future.

Description / Table of Contents: Slope tectonics: a short introduction / Michel Jaboyedoff, Giovanni B. Crosta and Doug Stead / Geological Society, London, Special Publications, 351, 1-10, 1 January 2011, https://doi.org/10.1144/SP351.1 --- Paraglacial gravitational deformations in the SW Alps: a review of field investigations, 10Be cosmogenic dating and physical modelling / S. El Bedoui, T. Bois, H. Jomard, G. Sanchez, T. Lebourg, E. Trics, Y. Guglielmi, S. Bouissou, A. Chemenda, Y. Rolland, M. Corsini and J. L. Pérez / Geological Society, London, Special Publications, 351, 11-25, 1 January 2011, https://doi.org/10.1144/SP351.2 --- Inheritance of ductile and brittle structures in the development of large rock slope instabilities: examples from western Norway / A. Saintot, I. H. C. Henderson and M.-H. Derron / Geological Society, London, Special Publications, 351, 27-78, 1 January 2011, https://doi.org/10.1144/SP351.3 --- Regional spatial variations in rockslide distribution from structural geology ranking: an example from Storfjorden, western Norway / Iain H. C. Henderson and Aline Saintot / Geological Society, London, Special Publications, 351, 79-95, 1 January 2011, https://doi.org/10.1144/SP351.4 --- Rock slope instabilities in Sogn and Fjordane County, Norway: a detailed structural and geomorphological analysis / Martina Böhme, Aline Saintot, Iain H. C. Henderson, Helge Henriksen and Reginald L. Hermanns / Geological Society, London, Special Publications, 351, 97-111, 1 January 2011, https://doi.org/10.1144/SP351.5 --- Controlling factors for deep-seated gravitational slope deformation (DSGSD) in the Aosta Valley (NW Alps, Italy) / G. Martinotti, D. Giordan, M. Giardino and S. Ratto / Geological Society, London, Special Publications, 351, 113-131, 1 January 2011, https://doi.org/10.1144/SP351.6 --- Palaeostress analysis of a giant Holocene rockslide near Boaco and Santa Lucia (Nicaragua, Central America) / Ivo Baron̆, Markéta Kernstocková, Roman Novotný, David Buriánek, Petr Hradecký, Pavel Havlic̆ek and Rostislav Melichar / Geological Society, London, Special Publications, 351, 133-145, 1 January 2011, https://doi.org/10.1144/SP351.7 --- Complex landslide behaviour and structural control: a three-dimensional conceptual model of Åknes rockslide, Norway / Michel Jaboyedoff, Thierry Oppikofer, Marc-Henri Derron, Lars Harald Blikra, Martina Böhme and Aline Saintot / Geological Society, London, Special Publications, 351, 147-161, 1 January 2011, https://doi.org/10.1144/SP351.8 --- Structural analysis of Turtle Mountain: origin and influence of fractures in the development of rock slope failures / Andrea Pedrazzini, Michel Jaboyedoff, Corey R. Froese, C. Willem Langenberg and Francisco Moreno / Geological Society, London, Special Publications, 351, 163-183, 1 January 2011, https://doi.org/10.1144/SP351.9 --- A structural, geomorphological and InSAR study of an active rock slope failure development / I. H. C. Henderson, T. R. Lauknes, P. T. Osmundsen, J. Dehls, Y. Larsen and T. F. Redfield / Geological Society, London, Special Publications, 351, 185-199, 1 January 2011, https://doi.org/10.1144/SP351.10 --- Numerical modelling of Plio-Quaternary slope evolution based on geological constraints: a case study from the Caramanico Valley (Central Apennines, Italy) / G. Bianchi Fasani, E. Di Luzio, C. Esposito, S. Martino and G. Scarascia-Mugnozza / Geological Society, London, Special Publications, 351, 201-214, 1 January 2011, https://doi.org/10.1144/SP351.11 --- Valley shape influence on deformation mechanisms of rock slopes / Christian Ambrosi and Giovanni B. Crosta / Geological Society, London, Special Publications, 351, 215-233, 1 January 2011, https://doi.org/10.1144/SP351.12 --- The Celentino deep-seated gravitational slope deformation (DSGSD): structural and geomechanical analyses (Peio Valley, NE Italy) / M. Ghirotti, S. Martin and R. Genevois / Geological Society, London, Special Publications, 351, 235-251, 1 January 2011, https://doi.org/10.1144/SP351.13 --- Megafans and outsize fans from catastrophic slope failures in Alpine glacial troughs: the Malser Haide and the Val Venosta cluster, Italy / David Jarman, Federico Agliardi and Giovanni B. Crosta / Geological Society, London, Special Publications, 351, 253-277, 1 January 2011, https://doi.org/10.1144/SP351.14

Description / Table of Contents: Understanding the sediments deposited by glaciers or other cold-climate processes assumes enhanced significance in the context of current global warming and the predicted melt and retreat of glaciers and ice sheets. This volume analyses glacial, proglacial and periglacial settings focusing, among others, on sedimentation at termini of tidewater glaciers, on hitherto not-well-understood high-mountain features, and on sediments such as slope and aeolian deposits whose clasts were sourced in glacial and periglacial regions, but have been transported and deposited by azonal processes. Difficulties are thus often encountered in inferring Pleistocene and pre-Pleistocene cold-climate conditions when the sedimentary record lacks many of the specific diagnostic indicators. The main objective of this volume is to establish the validity and limitations of the evidence that can be obtained from widely distributed clastic deposits, in order to achieve reliable palaeogeographic and palaeoclimatic reconstructions. At a more general level and on the much longer geological timescale, an understanding of ice-marginal and periglacial environments may better prepare us for the unavoidable reversal towards cooler and perhaps even glacial times in the future.

Description / Table of Contents: Professor Richard (Rick) Sibson revolutionized structural geology by illustrating that fault rocks contain an integrated record of earthquakes. Fault-rock textures develop in response to geological and physical variables such as composition, environmental conditions (e.g. temperature and pressure), fluid presence and strain rate. These parameters also determine the rate- and state-variable frictional stability of a fault, the dominant mineral deformation mechanism and shear strength, and ultimately control the partitioning between seismic and aseismic deformation. This volume contains a collection of papers that address the geological record of earthquake faulting from field-based or theoretical perspectives. The papers cover observations in active fault zones, the relationships between fault rocks and fault-slip styles, interpretation of fault-rock textures from the base of the seismogenic zone, consideration of the effects of fluids on faulting, discussion of fault reactivation v. initiation, and a review of future directions in geological earthquake research by Professor Sibson.

Description / Table of Contents: This volume brings together a collection of papers that summarize current ideas and recent progress in the study of granite-related mineralization systems. They provide a combination of field, experimental and theoretical studies. Papers are grouped according to the main granite-related ore systems: granite-pegmatite, skarn and greisen-veins, porphyry, orogenic gold, intrusion-related, epithermal and porphyry-related gold and base metal, iron oxide-copper-gold (IOCG), and special case studies. The studies provide a broad spread in terms of both space and time, highlighting granite-related ore deposits from Europe (Russia, Sweden, Croatia and Turkey), the Middle East (Iran), Asia (Japan and China) and South America (Brazil and Argentina) and spanning rocks from Palaeoproterozoic to Miocene in age.

Description / Table of Contents: Collision between Australia and SE Asia began in the Early Miocene and reduced the former wide ocean between them to a complex passage which connects the Pacific and Indian Oceans. Today, the Indonesian Throughflow passes through this gateway and plays an important role in global thermohaline flow. The surrounding region contains the maximum global diversity for many marine and terrestrial organisms. Reconstruction of this geologically complex region is essential for understanding its role in oceanic and atmospheric circulation, climate impacts, and the origin of its biodiversity. The papers in this volume discuss the Palaeozoic to Cenozoic geological background to Australia and SE Asia collision. They provide the background for accounts of the modern Indonesian Throughflow and oceanographic changes since the Neogene, and consider aspects of the region's climate history.

Description / Table of Contents: The latest Mars missions are returning data of unprecedented fidelity in their representation of the martian surface. New data include images with spatial resolution better than 30 cm per pixel, stereo imaging-derived terrain models with one meter postings, high-resolution imaging spectroscopy, and RADAR data that reveal subsurface structure. This book reveals how this information is being used to understand the evolution of martian landscapes, and includes topics such as fluvial flooding, permafrost and periglacial landforms, debris flows, deposition and erosion of sedimentary material, and the origin of lineaments on Phobos, the larger martian moon. Contemporary remote sensing data of Mars, on a par with those of Earth, reveal landscapes strikingly similar to regions of our own planet, so this book will be of interest to Earth scientists and planetary scientists alike. An overview chapter summarising Mars’ climate, geology and exploration is included for the benefit of those new to Mars.

Description / Table of Contents: Despite agreement on first-order features and mechanisms, critical aspects of the origin and evolution of the Tibetan Plateau, such as the exact timing and nature of collision, the initiation of plateau uplift, and the evolution of its height and width, are disputed, untested or unknown. This book gathers papers dealing with the growth and collapse of the Tibetan Plateau. The timing, the underlying mechanisms, their interactions and the induced surface shaping, contributing to the Tibetan Plateau evolution are tightly linked via coupled and feedback processes. We present interdisciplinary contributions allowing insight into the complex interactions between lithospheric dynamics, topography building, erosion, hydrological processes and atmospheric coupling. The book is structured in four parts: early processes in the plateau formation; recent growth of the Tibetan Plateau; mechanisms of plateau growth; and plateau uplift, surface processes and the monsoon.

Description / Table of Contents: The African continent preserves a long geological record that covers almost 75% of Earth's history. The Pan-Africanorogeny (c.600–500 Ma) brought together old continental kernels (West Africa, Congo, Kalahari and Tanzania) to form Gondwana and subsequently the supercontinent Pangaea by the late Palaeozoic. The break-up of Pangaea since the Jurassic and Cretaceous, primarily through opening of the Central Atlantic, Indian, and South Atlantic oceans, in combination with the complicated subduction history to the north, gradually shaped the African continent. This volume contains 18 contributions that discuss the geology of Africa from the Archaean to the present day. It celebrates African geology in two ways: first, it highlights multidisciplinary Earth science research by viewing the formation and evolution of Africa from 18 different angles; second, it celebrates the work of Kevin Burke and Lewis Ashwal and portrays the wide range of interests and research angles that have characterized these two scientists throughout their careers, working in Africa, and studying African geology.