ALBERT

Description / Table of Contents: The subduction zone volatile cycle is key to understanding the petrogenesis, transport, storage and eruption of arc magmas. Volatiles control the flux of slab components into the mantle wedge, are responsible for melt generation through lowering the solidi of mantle materials and influence the crystallizing phase assemblages in the overriding crust. Further, the rates and extents of degassing during magma storage and decompression affect magma rheology, ultimately control eruption style and have consequences for the environmental impact of explosive arc volcanism. This book highlights recent progress in constraining the role of volatiles in magmatic processes. Individual book sections are devoted to tracing volatiles from the subducting slab to the overriding crust, their role in subvolcanic processes and eruption triggering, as well as magmatic-hydrothermal systems and volcanic degassing. For the first time, all aspects of the overarching theme of volatile cycling are covered in detail within a single volume.

Description / Table of Contents: This Special Publication is dedicated to heritage stone: those natural stones that have special significance in human culture. Some stones that have had important uses in the past are now neglected because theyare no longer extracted. Others are still commercially important, but their heritage uses have not beenwell documented in widely available sources. The Heritage Stone Task Group of the International Unionof Geological Sciences is working to establish a new formal designation of 'Global Heritage StoneResource' to recognize those stones that have had internationally significant architectural and ornamentaluses. The aim is to spread awareness of the cultural heritage aspects of these stones, to help to encouragecontinued supply for maintenance and repair of important monuments and to preserve historically importantquarries. The aim is neither to promote nor to limit these stones for new construction: in some cases continuingcommercial use might help to ensure future supplies for building conservation purposes.

Description / Table of Contents: This volume provides a synopsis of current research on volcanic processes, as gained through the use ofpalaeomagnetic and rock magnetic techniques. Thermoremanent magnetization information provides apowerful means of deciphering thermal processes in volcanic deposits, including estimating the emplacementtemperature of pyroclastic deposits, which allows us to understand better the rates of coolingduring eruption and transport. Anisotropy of magnetic susceptibility and anisotropy of remanence areused primarily to investigate rock fabrics and to quantify flow dynamics in dykes, lava flows, and pyroclasticdeposits, as well as identify vent locations. Rock-magnetic characteristics allow correlation of volcanicdeposits, but also provide means to date volcanic deposits and to understand better their cooling history.Because lava flows are typically good recorders of past magnetic fields, data from them allow understandingof changes in geomagnetic field directions and intensity, providing clues on the origin of Earth's magneticfield.

Description / Table of Contents: The superposition of stratified rocks is an unmistakable manifestation of the history of sedimentary processes through deep time. However, the relationship between the preserved strata of the rock record and the passage of geological time, indisputable in principle, is unknowable in detail; incompleteness is an essential property of the record. That gaps exist at all scales in sedimentary successions is easily demonstrated from consideration of sediment accumulation rates, and expectations of continuity and completeness at any scale are correspondingly inadvisable. Locating and quantifying the gaps in the record is, however, very much less straightforward. Predictive modelling of strata - essential for their practical exploitation - requires such geohistorical understanding, yet over-simplified assumptions about how time is represented in rock can still lead to inadequate or even false conclusions. The contributions to this volume describe a range of practical studies, theoretical investigations, and numerical experiments in which the nature of the strata-time relationship is explored. Content: Strata and time: probing the gaps in our understanding -- Updating uniformitarianism: stratigraphy as just a set of 'frozen accidents' -- GSSPs, global stratigraphy and correlation -- Scaling laws for aggradation, denudation and progradation rates: the case for time-scale invariance at sediment sources and sinks -- The power-law attributes of stratigraphic layering and their possible significance -- The importance of doing nothing: stasis in sedimentation systems and its stratigraphic effects -- Investigating the occurrence of hierarchies of cyclicity in platform carbonates -- Cyclostratigraphy: data filtering as a source of spurious spectral peaks -- Stratigraphic continuity and fragmentary sedimentation: the success of cyclostratigraphy as part of integrated stratigraphy -- Synthesis of time-stratigraphic relationships and their impact on hydrocarbon reservoir distribution and performance, Bridport Sand Formation, Wessex Basin, UK -- 4D Wheeler diagrams: concept and applications -- Using the voids to fill tthe gaps: caves, time, and stratigraphy -- More gaps than shale: erosion of mud and its effect on preserved geochemical and palaeobiological signals -- More gap than record? Qualitative and quantitative assessment of stratigraphic gaps in a field based study, with examples from the Lower Silurian Pentamerus Beds of Shropshire, England and the Lower Ordovician Ribband Gp of County Wexford, Ireland -- British Pennsylvanian (Carboniferous) coal-bearing sequences: where is the time? -- Use of carbon accumulation rates to estimate the duration of coal seams and the influence of atmospheric dust deposition on coal composition.

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

Description / Table of Contents: This Special Publication will be an important tool for geoscientists, aimed at increasing the awareness of their societal role and responsibility in conducting education, research and practice activities.What are the responsibilities of a geoscientist ? And what motivations are needed to push geoscientists to practice the Earth sciences in an ethical way?The major environmental challenges affecting human communities require not only a strictly scientific and technical preparation by the geoscientists, but also a reflection on their broader obligations towards society. It is important that geoscientists consider geoethics as an indispensable framework on which to base their training and activity. The principles of geoethics can guide them to pursue the common good by weighing the benefits and costs of each choice, and identifying eco-friendly and society-friendly solutions that guarantee the respect of the right balance between human life and the dynamics of the Earth.Communication and dissemination of geosciences should become core activities in building a knowledge-based society, which is able better to protect itself and the Earth ecosystems in order to guarantee a life in harmony with our planet for future generations.

Description / Table of Contents: Exploration of subsurface Antarctica: uncovering past changes and modern processes / Martin J. Siegert, Stewart S. R. Jamieson and Duanne White / Geological Society, London, Special Publications, 461, 1-6, 25 September 2017, https://doi.org/10.1144/SP461.15 --- A 60-year international history of Antarctic subglacial lake exploration / Martin J. Siegert / Geological Society, London, Special Publications, 461, 7-21, 25 May 2017, https://doi.org/10.1144/SP461.5 --- Exploring the Recovery Lakes region and interior Dronning Maud Land, East Antarctica, with airborne gravity, magnetic and radar measurements / Rene Forsberg, Arne V. Olesen, Fausto Ferraccioli, Tom A. Jordan, Kenichi Matsuoka, Andres Zakrajsek, Marta Ghidella and Jamin S. Greenbaum / Geological Society, London, Special Publications, 461, 23-34, 20 September 2017, https://doi.org/10.1144/SP461.17 --- Ice-flow reorganization within the East Antarctic Ice Sheet deep interior / L. H. Beem, M. G. P. Cavitte, D. D. Blankenship, S. P. Carter, D. A. Young, G. R. Muldoon, C. S. Jackson and M. J. Siegert / Geological Society, London, Special Publications, 461, 35-47, 11 August 2017, https://doi.org/10.1144/SP461.14 --- Was South Georgia covered by an ice cap during the Last Glacial Maximum? / Duanne A. White, Ole Bennike, Martin Melles, Sonja Berg and Steven A. Binnie / Geological Society, London, Special Publications, 461, 49-59, 13 June 2017, https://doi.org/10.1144/SP461.4 --- The Gebra–Magia Complex: mass-transport processes reworking trough-mouth fans in the Central Bransfield Basin (Antarctica) / D. Casas, M. García, F. Bohoyo, A. Maldonado and G. Ercilla / Geological Society, London, Special Publications, 461, 61-75, 16 June 2017, https://doi.org/10.1144/SP461.10 --- Bathymetry of Schirmacher lakes as a tool for geomorphological evolution studies / Ashit Kumar Swain / Geological Society, London, Special Publications, 461, 77-93, 11 July 2017, https://doi.org/10.1144/SP461.13 --- Heavy mineral assemblage of marine sediments as an indicator of provenance and east antarctic ice sheet fluctuations / Mayuri Pandey, Naresh C. Pant, Paromita Biswas, Prakash K. Shrivastava, Sonalika Joshi and Neety Nagi / Geological Society, London, Special Publications, 461, 95-111, 22 June 2017, https://doi.org/10.1144/SP461.2 --- Position and variability of complex structures in the central East Antarctic Ice Sheet / Thilo Wrona, Michael J. Wolovick, Fausto Ferraccioli, Hugh Corr, Tom Jordan and Martin J. Siegert / Geological Society, London, Special Publications, 461, 113-129, 15 June 2017, https://doi.org/10.1144/SP461.12 --- Summit of the East Antarctic Ice Sheet underlain by thick ice-crystal fabric layers linked to glacial–interglacial environmental change / Bangbing Wang, Bo Sun, Carlos Martin, Fausto Ferraccioli, Daniel Steinhage, Xiangbin Cui and Martin J. Siegert / Geological Society, London, Special Publications, 461, 131-143, 26 May 2017, https://doi.org/10.1144/SP461.1 --- Drilling project at Gamburtsev Subglacial Mountains, East Antarctica: recent progress and plans for the future / Pavel Talalay, Youhong Sun, Yue Zhao, Yuansheng Li, Pinlu Cao, Alexey Markov, Huiwen Xu, Rusheng Wang, Nan Zhang, Xiaopeng Fan, Yang Yang, Mikhail Sysoev, Yongwen Liu and Yunchen Liu / Geological Society, London, Special Publications, 461, 145-159, 24 May 2017, https://doi.org/10.1144/SP461.9 --- A deep subglacial embayment adjacent to the grounding line of Institute Ice Stream, West Antarctica / Hafeez Jeofry, Neil Ross, Hugh F. J. Corr, Jilu Li, Prasad Gogineni and Martin J. Siegert / Geological Society, London, Special Publications, 461, 161-173, 13 June 2017, https://doi.org/10.1144/SP461.11 --- Ocean forced variability of Totten Glacier mass loss / Jason Roberts, Benjamin K. Galton-Fenzi, Fernando S. Paolo, Claire Donnelly, David E. Gwyther, Laurie Padman, Duncan Young, Roland Warner, Jamin Greenbaum, Helen A. Fricker, Antony J. Payne, Stephen Cornford, Anne Le Brocq, Tas van Ommen, Don Blankenship and Martin J. Siegert / Geological Society, London, Special Publications, 461, 175-186, 23 August 2017, https://doi.org/10.1144/SP461.6 --- Chemical characteristics of the ice cores obtained after the first unsealing of subglacial Lake Vostok / Irina Alekhina, Alexey Ekaykin, Alexey Moskvin and Vladimir Lipenkov / Geological Society, London, Special Publications, 461, 187-196, 24 May 2017, https://doi.org/10.1144/SP461.3 --- Antarctic subglacial groundwater: a concept paper on its measurement and potential influence on ice flow / Martin J. Siegert, Bernd Kulessa, Marion Bougamont, Poul Christoffersen, Kerry Key, Kristoffer R. Andersen, Adam D. Booth and Andrew M. Smith / Geological Society, London, Special Publications, 461, 197-213, 25 May 2017, https://doi.org/10.1144/SP461.8 --- Modern to Glacial age subglacial meltwater drainage at Law Dome, coastal East Antarctica from topography, sediments and jökulhlaup observations / Ian D. Goodwin, Jason L. Roberts, David M. Etheridge, John Hellstrom, Andrew D. Moy, Marta Ribo and Andrew M. Smith / Geological Society, London, Special Publications, 461, 215-230, 12 July 2017, https://doi.org/10.1144/SP461.16 --- A new volcanic province: an inventory of subglacial volcanoes in West Antarctica / Maximillian van Wyk de Vries, Robert G. Bingham and Andrew S. Hein / Geological Society, London, Special Publications, 461, 231-248, 29 May 2017, https://doi.org/10.1144/SP461.7

Description / Table of Contents: The rivers of East Asia are some of the largest and most important to human society and the global economy. They drain a variety of terrains from the Tibetan plateau, the hill country of southern China and the steep mountains of Taiwan. The sediment they carry potentially records the long-term evolution of continental environments within the marine stratigraphic record. Sediments reaching the ocean have to traverse the wide continental shelves where they may be reworked and transported by longshore currents, typhoon storm waves, as well as large ocean currents such as the Kuroshio. Deciphering any marine record requires us to understand the dynamics of sediment transport on the continental shelves, and this region acts as a global type example of such processes. Studies in this volume span a wide range of subdisciplines in the marine sciences and provide new insights into how sediment is distributed offshore after leaving the river mouths.

Description / Table of Contents: Abstract The Palaeozoic Era ends with the c. 47-million-year-long Permian Period. This was a major juncture in Earth history when the vast Pangean supercontinent continued its assembly and the global biota suffered the most extensive biotic decimation of the Phanerozoic, the end-Permian mass extinction. It was also the time of accumulation of vast mineral and energy deposits, notably of salt and petroleum. The temporal ordering of geological and biotic events during Permian time is, therefore, critical to the interpretation of some unique and pivotal events in Earth history. This temporal ordering is based mostly on the Permian timescale, which has been developed and refined for nearly two centuries. This book reviews the history of the development of the Permian chronostratigraphic scale. It also includes comprehensive analyses of Permian radioisotopic ages, magnetostratigraphy, isotope-based correlations, and timescale-relevant marine and non-marine biostratigraphy and biochronology.

Description / Table of Contents: Abstract In Earth evolution, mountain belts are the loci of crustal growth, reworking and recycling. These crustal-scale processes are unravelled through microscale investigations of textures and mineral assemblages of metamorphic rocks. Multiple episodes of metamorphism, re-equilibration and deformation, however, generally produce a complex and tightly interwoven pattern of microstructures and assemblages. Over the last two decades, the combination of advanced computing and technological capabilities with new concepts has provided a vast array of novel petrological tools and high-resolution/high-sensitivity techniques for microanalysis and imaging. Such novel approaches are proving fundamental to untangling the enigma represented by metamorphism with an unprecedented level of detail and confidence. As a result, the first decade and a half of this century has already seen the tumultuous development of new research avenues in metamorphic petrology. This book aims to provide a timely overview of the state of the art of this field, of newly developed petrological techniques, future advancements and significant new case studies.

Description / Table of Contents: Abstract This volume comprises 17 contributions that address the architecture and geodynamic evolution of the Himalaya–Karakoram–Tibet (HKT) system, covering wide aspects, from the active seismicity of the present day to the remnants of the Proterozoic orogen. The articles investigate the HKT system at different scales, blending field research with laboratory studies. The role of various lithospheric components and their inheritance in the geodynamic and magmatic evolution of the HKT system through time, and their links to global geological events, are studied in the field. The laboratory research focuses on the (sub-)micrometre scale, detailing micro-structural geology, crystal chemistry, geochronology, and the study of circulating fluids, their preservation (trapped in fluid inclusions) and their evolution, distribution, migration and interaction with the solid host. An orogen over 2000 km long can be understood only if the processes at the nanometre and micrometre scales are taken into account. The contributions in this volume successfully combine these scales to enhance our understanding of the HKT system.

Description / Table of Contents: Fifty years ago, Tuzo Wilson published his paper asking ‘Did the Atlantic close and then re-open?’. This led to the ‘Wilson Cycle’ concept in which the repeated opening and closing of ocean basins along old orogenic belts is a key process in the assembly and breakup of supercontinents. The Wilson Cycle underlies much of what we know about the geological evolution of the Earth and its lithosphere, and will no doubt continue to be developed as we gain more understanding of the physical processes that control mantle convection, plate tectonics, and as more data become available from currently less accessible regions. This volume includes both thematic and review papers covering various aspects of the Wilson Cycle concept. Thematic sections include: (1) the Classic Wilson v. Supercontinent Cycles, (2) Mantle Dynamics in the Wilson Cycle, (3) Tectonic Inheritance in the Lithosphere, (4) Revisiting Tuzo's question on the Atlantic, (5) Opening and Closing of Oceans, and (6) Cratonic Basins and their place in the Wilson Cycle.

Description / Table of Contents: Precipitation as the central meteorological feature for agriculture, water security, and human well-being amongst others, has gained special attention ever since. Lack of precipitation may have devastating effects such as crop failure and water scarcity. Abundance of precipitation, on the other hand, may as well result in hazardous events such as flooding and again crop failure. Thus, great effort has been spent on tracking changes in precipitation and relating them to underlying processes. Particularly in the face of global warming and given the link between temperature and atmospheric water holding capacity, research is needed to understand the effect of climate change on precipitation. The present work aims at understanding past changes in precipitation and other meteorological variables. Trends were detected for various time periods and related to associated changes in large-scale atmospheric circulation. The results derived in this thesis may be used as the foundation for attributing changes in floods to climate change.…

Description / Table of Contents: Abstract This Special Publication highlights the importance of clays and clayey material, and their multiple roles, in many national geological disposal facilities for higher activity radioactive wastes. Clays can be both the disposal facility host rock and part of its intrinsic engineered barriers, and may be present in the surrounding geological environment. Clays possess various characteristics that make them high-quality barriers to the migration of radionuclides and chemical contaminants, e.g. very little water movement, diffusive transport, retention capacity, self-sealing capacity, stability over millions of years, homogeneity and lateral continuity. The 20 papers presented in this Special Publication cover a range of topics related to clays in radioactive waste confinement. Aspects of clay characterization and behaviour at various temporal and spatial scales relevant to the confinement of radionuclides in clay are discussed, from phenomenological processes to the overall understanding of the performance and safety of geological disposal facilities.

Description / Table of Contents: According to the classical plume hypothesis, mantle plumes are localized upwellings of hot, buoyant material in the Earth’s mantle. They have a typical mushroom shape, consisting of a large plume head, which is associated with the formation of voluminous flood basalts (a Large Igneous Province) and a narrow plume tail, which generates a linear, age-progressive chain of volcanic edifices (a hotspot track) as the tectonic plate migrates over the relatively stationary plume. Both plume heads and tails reshape large areas of the Earth’s surface over many tens of millions of years. However, not every plume has left an exemplary record that supports the classical hypothesis. The main objective of this thesis is therefore to study how specific hotspots have created the crustal thickness pattern attributed to their volcanic activities. Using regional geodynamic models, the main chapters of this thesis address the challenge of deciphering the three individual (and increasingly complex) Réunion, Iceland, and Kerguelen hotspot histories,…

Description / Table of Contents: Geomaterials derived from the Earth's crust and used in construction after appropriate processing are among the earliest raw materials exploited, processed and used by humans. Their numerous functional properties include accessibility, workability and serviceability, and these are explored within this volume. In modern society, sustainable use of raw materials, specifically those exploited in large volumes such as geomaterials for construction, raises questions of reducing extraction of primary resources and thus minimizing impacts on natural systems, and also employment of materials and technologies to lower emissions of deleterious substances into the atmosphere. This will be possible only if we fully understand the properties, processing and mode of use of traditional geomaterials. Although most of the papers within this volume were written by geologists, the contributions will also be of interest to those working in cultural heritage, monument conservation, civil engineering and architecture.

Description / Table of Contents: Abstract The history of the European oil and gas industry reflects local as well as global political events, economic constraints and the personal endeavours of individual petroleum geoscientists as much as it does the development of technologies and the underlying geology of the region. The first commercial oil wells in Europe were drilled in Poland in 1853, Romania in 1857, Germany in 1859 and Italy in 1860. The 23 papers in this volume focus on the history and heritage of the oil and gas industry in the key European oil-producing countries from the earliest onshore drilling to its development into the modern industry that we know today. The contributors chronicle the main events and some of the major players that shaped the industry in Europe. The volume also marks several important anniversaries, including 150 years of oil exploration in Poland and Romania, the centenary of the drilling of the first oil well in the UK and 50 years of oil production from onshore Spain.

Description / Table of Contents: Abstract Economically viable concentrations of mineral resources are uncommon in Earth's crust. Most ore deposits that were mined in the past or are currently being extracted were found at or near Earth's surface, often serendipitously. To meet the future demand for mineral resources, exploration success hinges on identifying targets at depth. Achieving this requires accurate and informed models of the Earth's crust that are consistent with all available geological, geochemical and geophysical information, paired with an understanding of how ore-forming systems relate to Earth's evolving structure. Contributions to this volume address the future resources challenge by (i) applying advanced microscale geochemical detection and characterization methods, (ii) introducing more rigorous 3D Earth models, (iii) exploring critical behaviour and coupled processes, (iv) evaluating the role of geodynamic and tectonic setting and (v) applying 3D structural models to characterize specific ore-forming systems.

Description / Table of Contents: The Yukon Coast in Canada is an ice-rich permafrost coast and highly sensitive to changing environmental conditions. Retrogressive thaw slumps are a common thermoerosion feature along this coast, and develop through the thawing of exposed ice-rich permafrost on slopes and removal of accumulating debris. They contribute large amounts of sediment, including organic carbon and nitrogen, to the nearshore zone. The objective of this study was to 1) identify the climatic and geomorphological drivers of sediment-meltwater release, 2) quantify the amount of released meltwater, sediment, organic carbon and nitrogen, and 3) project the evolution of sediment-meltwater release of retrogressive thaw slumps in a changing future climate. The analysis is based on data collected over 18 days in July 2013 and 18 days in August 2012. A cut-throat flume was set up in the main sediment-meltwater channel of the largest retrogressive thaw slump on Herschel Island. In addition, two weather stations, one on top of the undisturbed tundra and one on the…

Description / Table of Contents: The Himalayas are a region that is most dependent, but also frequently prone to hazards from changing meltwater resources. This mountain belt hosts the highest mountain peaks on earth, has the largest reserve of ice outside the polar regions, and is home to a rapidly growing population in recent decades. One source of hazard has attracted scientific research in particular in the past two decades: glacial lake outburst floods (GLOFs) occurred rarely, but mostly with fatal and catastrophic consequences for downstream communities and infrastructure. Such GLOFs can suddenly release several million cubic meters of water from naturally impounded meltwater lakes. Glacial lakes have grown in number and size by ongoing glacial mass losses in the Himalayas. Theory holds that enhanced meltwater production may increase GLOF frequency, but has never been tested so far. The key challenge to test this notion are the high altitudes of 〉4000 m, at which lakes occur, making field work impractical. Moreover, flood waves can attenuate rapidly in mountain channels downstream, so that many GLOFs have likely gone unnoticed in past decades. Our knowledge on GLOFs is hence likely biased towards larger, destructive cases, which challenges a detailed quantification of their frequency and their response to atmospheric warming. Robustly quantifying the magnitude and frequency of GLOFs is essential for risk assessment and management along mountain rivers, not least to implement their return periods in building design codes. [...]

Description / Table of Contents: Tectonic and climatic boundary conditions determine the amount and the characteristics (size distribution and composition) of sediment that is generated and exported from mountain regions. On millennial timescales, rivers adjust their morphology such that the incoming sediment (Qs,in) can be transported downstream by the available water discharge (Qw). Changes in climatic and tectonic boundary conditions thus trigger an adjustment of the downstream river morphology. Understanding the sensitivity of river morphology to perturbations in boundary conditions is therefore of major importance, for example, for flood assessments, infrastructure and habitats. Although we have a general understanding of how rivers evolve over longer timescales, the prediction of channel response to changes in boundary conditions on a more local scale and over shorter timescales remains a major challenge. To better predict morphological channel evolution, we need to test (i) how channels respond to perturbations in boundary conditions and (ii) how signals ...

Description / Table of Contents: The concept of hydrologic connectivity summarizes all flow processes that link separate regions of a landscape. As such, it is a central theme in the field of catchment hydrology, with influence on neighboring disciplines such as ecology and geomorphology. It is widely acknowledged to be an important key in understanding the response behavior of a catchment and has at the same time inspired research on internal processes over a broad range of scales. From this process-hydrological point of view, hydrological connectivity is the conceptual framework to link local observations across space and scales. This is the context in which the four studies this thesis comprises of were conducted. The focus was on structures and their spatial organization as important control on preferential subsurface flow. Each experiment covered a part of the conceptualized flow path from hillslopes to the stream: soil profile, hillslope, riparian zone, and stream. For each study site, the most characteristic structures of the investigated domain and scale, such as slope deposits and peat layers were identified based on preliminary or previous investigations or literature reviews. Additionally, further structural data was collected and topographical analyses were carried out. [...]

Description / Table of Contents: Abstract The challenges facing submarine mass movement researchers and engineers are plentiful and exciting. This book follows several high-profile submarine landslide disasters that have reached the world's attention over the past few years. For decades, researchers have been mapping the world's mass movements. Their significant impacts on the Earth by distributing sediment on phenomenal scales is undeniable. Their importance in the origins of buried resources has long been understood. Their hazard potential ranges from damaging to apocalyptic, frequently damaging local infrastructure and sometimes devastating whole coastlines. Moving beyond mapping advances, the subaqueous mass movement scientists and practitioners are now also focussed on assessing the consequences of mass movements, and the measurement and modelling of events, hazard analysis and mitigation. Many state-of-the-art examples are provided in this book, which is produced under the auspices of the United Nations Educational, Scientific and Cultural Organisation Program S4SLIDE (Significance of Modern and Ancient Submarine Slope LandSLIDEs).

Description / Table of Contents: This Special Publication is dedicated to heritage stone: those natural stones that have special significance in human culture. Some stones that have had important uses in the past are now neglected because theyare no longer extracted. Others are still commercially important, but their heritage uses have not beenwell documented in widely available sources. The Heritage Stone Task Group of the International Unionof Geological Sciences is working to establish a new formal designation of 'Global Heritage StoneResource' to recognize those stones that have had internationally significant architectural and ornamentaluses. The aim is to spread awareness of the cultural heritage aspects of these stones, to help to encouragecontinued supply for maintenance and repair of important monuments and to preserve historically importantquarries. The aim is neither to promote nor to limit these stones for new construction: in some cases continuingcommercial use might help to ensure future supplies for building conservation purposes.

Description / Table of Contents: Abstract Reservoir quality is studied using a wide range of similar techniques in both sandstones and carbonates. Sandstone and carbonate reservoir quality both benefit from the study of modern analogues and experiments, but modelling approaches are currently quite different for these two types of reservoirs. There are many common controls on sandstone and carbonate reservoir quality, but also distinct differences due primarily to mineralogy. Numerous controversies remain including the question of oil inhibition, the key control on pressure solution and geochemical flux of material to or from reservoirs. This collection of papers contains case-study-based examples of sandstone and carbonate reservoir quality prediction as well as modern analogue, outcrop analogue, modelling and advanced analytical approaches.

Description / Table of Contents: Abstract Karst landscapes and karst aquifers are composed of a variety of soluble rocks, such as salt, gypsum, anhydrite, limestone, dolomite and quartzite. They are fascinating areas of exploration, study and research. As karst rocks are abundant on the Earth's surface, the fast evolution of karst landscapes and the rapid flow of water through karst aquifers present many challenges from a number of different perspectives. This collection of 25 papers deals with different aspects of these challenges, including karst geology, geomorphology and speleogenesis, karst hydrogeology, karst modelling, and karst hazards and management. Together these papers provide a state-of-the-art review of the current challenges and solutions we face in describing karst from a scientific perspective, while at the same time providing useful data and information for managing karst territories to land planners, developers, and managers of show caves, natural parks and reserves in karst terrains.

Description / Table of Contents: In the last decades the frequency and intensity of extreme weather events like heat waves and heavy rainfall have increased and are at least partly linked to global warming. These events can have a strong impact on agricultural and economic production and, thereby, on society. Thus, it is important to improve our understanding of the physical processes leading to those extreme events in order to provide accurate near-term and long-term forecasts. Thermodynamic drivers associated with global warming are well understood, but dynamical aspects of the atmosphere much less so. The dynamical aspects, while less important than the thermodynamic drivers in regards to large-scale and long-time averaged effects, play a critical role in the formation of extremes. The overall aim of this thesis is to improve our understanding of patterns, variability and trends in the global atmospheric circulation under a changing climate. In particular, in this dissertation I developed two new data-driven methods to quantitatively describe the dynamics of…

Description / Table of Contents: Abstract The Black Sea remains one of the largest underexplored rift basins in the world. Future success is dependent on a better understanding of a number of geological uncertainties. These include reservoir and source rock presence and quality, and the timing of migration of hydrocarbons relative to trap formation. An appreciation of the geological history of the Black Sea basins and the surrounding orogens is therefore key. The timing of basin formation, uplift of the margins, and of facies distribution remain issues for robust debate. This Special Publication presents the results of 15 studies that relate to the tectono-stratigraphy and petroleum geology of the Black Sea. The methodologies of these studies encompass crustal structure, geodynamic evolution, stratigraphy and its regional correlation, petroleum systems, source to sink, hydrocarbon habitat and play concepts, and reviews of past exploration. They provide insight into the many ongoing controversies concerning Black Sea regional geology and provide a better understanding of the geological risks that must be considered for future hydrocarbon exploration.

Description / Table of Contents: The Himalaya–Karakoram–Tibet mountain belt resulted from Cenozoic collision of India and Asia and is frequently used as the type example of a continental collision orogenic belt. The last quarter of a century has seen the publication of a remarkably detailed dataset relevant to the evolution of this belt. Detailed fieldwork backed up by state-of-the-art structural analysis, geochemistry, mineral chemistry, igneous and metamorphic petrology, isotope chemistry, sedimentology and geophysics produced a wide-ranging archive of data-rich scientific papers. The rationale for this book is to provide a coherent overview of these datasets in addressing the evolution of the mountain ranges we see today. This volume comprises 21 specially invited review papers on the Himalaya, Kohistan arc, Tibet, the Karakoram and Pamir ranges. These papers span the history of Himalayan research, chronology of the collision, stratigraphy, magmatic and metamorphic processes, structural geology and tectonics, seismicity, geophysics, and the evolution of the Indian monsoon. This landmark set of papers should underpin the next 25 years of Himalayan research.

Description / Table of Contents: Permafrost, defined as ground that remains frozen for at least two consecutive years, is a prominent feature of polar regions. In the Northern Hemisphere, approximately 23 million km2 of the ground are affected by permafrost. Climatic warming, which has a greater effect on the Arctic than on any other region on Earth, leads to permafrost thaw, caused by gradual deepening of the seasonal unfrozen layer (active layer), thermokarst formation (i.e. land subsidence due to ground ice loss) and thermo-erosion. In the course of thaw, formerly freeze-locked organic carbon (OC) is mobilized and mineralized into greenhouse gases (GHGs), fostering further climate warming – a process known as permafrost carbon feedback. Current climate models focus on GHG release from gradual deepening of the active layer and neglect the OC turnover during lateral transport induced by thermokarst and abrupt thermo-erosion. As such, the accelerated erosion of Arctic permafrost coasts, which make up ~34 % of the global coasts, deliver vast amounts of OC into the Arctic Ocean. However, little is known about the amounts of labile and fast bioavailable dissolved OC (DOC), the impact of thermokarst on mobilized organic matter (OM) characteristics, and the release of GHGs from eroding permafrost coasts. To fill that knowledge gap, the main objectives of the thesis are to investigate (i) how much DOC is mobilized from coastal erosion, (ii) how thermokarst and -erosion alters OM characteristics upon thaw on transit to the ocean, and (iii) how much GHGs are emitted from the nearshore zones of eroding permafrost coasts. Field work and sampling took place along the Yukon coast and on Qikiqtaruk (Herschel Island) in the western Canadian Arctic. An interdisciplinary approach was used to quantify OM (OC and nitrogen) as well as to identify degradation processes. The methods used included sedimentology, geo- and hydrochemistry, remote sensing, statistical analyses, and gas chromatography. The thesis shows that considerable amounts of DOC are released from eroding permafrost coasts. Although OC fluxes into the ocean are dominated by DOC from Arctic rivers and particulate OC (POC), labile DOC derived from permafrost plays an important role as it is quickly available for biogeochemical cycling and turnover into GHGs. During transit from land to ocean OM characteristics are substantially altered by thermokarst formation and thermo-erosion. In mudpools, originating from in-situ thawed permafrost, as well as in thaw streams draining thermokarst features towards the ocean, mobilized OM issubject to dilution with melted ground ice and degradation, which result in a decrease of OM contents by more than 50 %. The turnover of OC continues in the nearshore zone. The biochemically most labile OC portions are rapidly lost within months and mineralized into GHGs. The production of GHGs in the ocean is 60 to 80 % as efficient as on land and primarily in form of carbon dioxide (CO2), due to aerobic conditions in the nearshore zone. During each open water season in the Arctic approximately 0.7 to 1.2 Tg of CO2 are emitted from the coastal fringe. The remaining OM is buried in nearshore and shelf sediments, potentially remobilized by waves, currents and ice scouring at later stages. To conclude, the thesis shows that eroding permafrost coasts release large amounts of OC, from which considerable portions are labile DOC. In the course of thermokarst formation and thermo-erosion, OM is diluted and the most labile portions subject to rapid turnover into GHGs. This shows that eroding permafrost coasts are a major yet neglected source of CO2 to the atmosphere. With increasing temperatures and longer sea ice-free conditions projected for the Arctic, the erosion of permafrost coasts accelerates. Consequently, the transfer of OC to the ocean accompanied by GHG production increases, which is expected to have drastic impacts for the climate and coastal ecosystems.

Description / Table of Contents: Steep mountain channels are an important component of the fluvial system. On geological timescales, they shape mountain belts and counteract tectonic uplift by erosion. Their channels are strongly coupled to hillslopes and they are often the main source of sediment transported downstream to low-gradient rivers and to alluvial fans, where commonly settlements in mountainous areas are located. Hence, mountain streams are the cause for one of the main natural hazards in these regions. Due to climate change and a pronounced populating of mountainous regions the attention given to this threat is even growing. Although quantitative studies on sediment transport have significantly advanced our knowledge on measuring and calibration techniques we still lack studies of the processes within mountain catchments. Studies examining the mechanisms of energy and mass exchange on small temporal and spatial scales in steep streams remain sparse in comparison to low-gradient alluvial channels. In the beginning of this doctoral project, a vast ...

Description / Table of Contents: Active and passive source data from two seismic experiments within the interdisciplinary project TIPTEQ (from The Incoming Plate to mega Thrust EarthQuake processes) were used to image and identify the structural and petrophysical properties (such as P- and S-velocities, Poisson's ratios, pore pressure, density and amount of fluids) within the Chilean seismogenic coupling zone at 38.25°S, where in 1960 the largest earthquake ever recorded (Mw 9.5) occurred. Two S-wave velocity models calculated using traveltime and noise tomography techniques were merged with an existing velocity model to obtain a 2D S-wave velocity model, which gathered the advantages of each individual model. In a following step, P- and S-reflectivity images of the subduction zone were obtained using different pre stack and post-stack depth migration techniques. Among them, the recent prestack line-drawing depth migration scheme yielded revealing results. Next, synthetic seismograms modelled using the reflectivity method allowed, through their input 1D synthetic P- and S-velocities, to infer the composition and rocks within the subduction zone. Finally, an image of the subduction zone is given, jointly interpreting the results from this work with results from other studies. The Chilean seismogenic coupling zone at 38.25°S shows a continental crust with highly reflective horizontal, as well as (steep) dipping events. Among them, the Lanalhue Fault Zone (LFZ), which is interpreted to be east-dipping, is imaged to very shallow depths. ...

Description / Table of Contents: In the Highlands of Sri Lanka, erosion and chemical weathering rates are among the lowest for global mountain denudation. In this tropical humid setting, highly weathered deep saprolite profiles have developed from high-grade metamorphic charnockite during spheroidal weathering of the bedrock. The spheroidal weathering produces rounded corestones and spalled rindlets at the rock-saprolite interface. I used detailed textural, mineralogical, chemical, and electron-microscopic (SEM, FIB, TEM) analyses to identify the factors limiting the rate of weathering front advance in the profile, the sequence of weathering reactions, and the underlying mechanisms. The first mineral attacked by weathering was found to be pyroxene initiated by in situ Fe oxidation, followed by in situ biotite oxidation. Bulk dissolution of the primary minerals is best described with a dissolution – re-precipitation process, as no chemical gradients towards the mineral surface and sharp structural boundaries are observed at the nm scale. Only the local oxidation in pyroxene and biotite is better described with an ion by ion process. The first secondary phases are oxides and amorphous precipitates from which secondary minerals (mainly smectite and kaolinite) form. Only for biotite direct solid state transformation to kaolinite is likely. [...]

Description / Table of Contents: Abstract High pressure (HP) and ultrahigh pressure (UHP) metamorphic rocks play a key role in understanding the tectonic evolution of orogenic belts. They have typically experienced complex changes during subduction and exhumation processes arising from recrystallization, deformation, fluid–rock interactions and even partial melting, and may therefore carry valuable records of evolving geodynamic systems in an orogenic belt. This special publication addresses the current work on HP–UHP metamorphism and its relation to the tectonic evolution of orogenic belts. This special publication contains fifteen papers covering the important orogenic belts of the Himalaya, Dabie–Sulu, Tian Shan, North Qaidam and others that have been grouped into three parts: (I) new developments in the determination of metamorphic pressure–temperature (PT) conditions and their timing, (II) overview papers of well-known HP–UHP metamorphic belts and (III) research papers for some newly discovered HP–UHP belts.

Description / Table of Contents: Abstract Understanding the sedimentary and geophysical archive of glaciated margins is a complex task that requires integration and analysis of disparate sedimentological and geophysical data. Their analysis is vital for understanding the dynamics of past ice sheets and how they interact with their neighbouring marine basins, on timescales that cannot be captured by observations of the cryosphere today. As resources, sediments deposited on the inner margins of glaciated shelves also exhibit resource potential where more sand-dominated systems occur, acting as reservoirs for both hydrocarbons and water. This book surveys the full gamut of glaciated margins, from deep time (Neoproterozoic, Ordovician and Carboniferous–Permian) to modern high-latitude margins in Canada and Antarctica. This collection of papers is the first attempt to deliberately do this, allowing not only the similarities and differences between modern and ancient glaciated margins to be explored, but also the wide spectrum of their mechanisms of investigation to be probed. Together, these papers offer a high-resolution, spatially and temporally diverse blueprint of the depositional processes, ice sheet dynamics, and basin architectures of the world's former glaciated margins; a vital resource in advancing understanding of our present and future marine-terminating ice sheet margins.

Description / Table of Contents: Die Arktis erwärmt sich schneller als der Rest der Erde. Die Auswirkungen manifestieren sich unter Anderem in einer verstärkten Erwärmung der arktischen Grenzschicht. Diese Arbeit befasst sich mit Wechselwirkungen zwischen synoptischen Zyklonen und der arktischen Atmosphäre auf lokalen bis überregionalen Skalen. Ausgangspunkt dafür sind Messdaten und Modellsimulationen für den Zeitraum der N-ICE2015 Expedition, die von Anfang Januar bis Ende Juni 2015 im arktischen Nordatlantiksektor stattgefunden hat. Anhand von Radiosondenmessungen lassen sich Auswirkungen von synoptischen Zyklonen am deutlichsten im Winter erkennen, da sie durch die Advektion warmer und feuchter Luftmassen in die Arktis den Zustand der Atmosphäre von einem strahlungs-klaren in einen strahlungs-opaken ändern. Obwohl dieser scharfe Kontrast nur im Winter existiert, zeigt die Analyse, dass der integrierte Wasserdampf als Indikator für die Advektion von Luftmassen aus niedrigen Breiten in die Arktis auch im Frühjahr geeignet ist. Neben der Advektion von…

Description / Table of Contents: Our understanding of the physical and chemical processes that regulate the evolution of magmatic systems has improved tremendously since the foundations were laid down 100 years ago by Bowen. The concept of crustal magma chambers has progressively evolved from molten-rock vats to thermally, chemically and physically heterogeneous reservoirs that are kept active by the periodic injection of magma. This new model, while more complex, provides a better framework to interpret volcanic activity and decipher the information contained in intrusive and extrusive rocks. Igneous/metamorphic petrology, geochemistry, geochronology and numerical modelling all contributed towards this new picture of crustal magmatic systems. This book provides an overview of the wide range of approaches that can nowadays be used to understand the chemical, physical and temporal evolution of magmatic and volcanic systems.

Description / Table of Contents: Abstract The Southern Permian Basin, as its name suggests, is a historical heartland for hydrocarbon production from the Palaeozoic Rotliegend interval. However, in this mature basin the Mesozoic presents further possibilities to offer resource security to NW Europe. Such opportunities include increasing efficiency in the production of discovered hydrocarbons, exploration for further hydrocarbons (both conventional and unconventional) and efficient exploration for, and production of, geothermal energy. All these potential resources require a grounding in technically sound geoscience, via traditional scientific observation and the application of new technologies, to unlock their value. The main aim of this volume is to bring together the work of academics and industry workers to consider cross-border geoscience including contributions on Poland, Germany, The Netherlands, the United Kingdom and adjacent areas. The work presented intends to contribute to the development and discovery of further Mesozoic energy resources across the basin.

Description / Table of Contents: Abstract Alluvial and fluvial fans are the most widespread depositional landform bordering the margins of highland regions and actively subsiding continental basins, across a broad spectrum of tectonic and climatic settings. They are significant to the local morphodynamics of mountain regions and also to the evolution of sediment-routing systems, affecting the propagation and preservation of stratigraphic signals of environmental change over vast areas. The volume presents case studies discussing the geology and geomorphology of alluvial and fluvial fans from both active systems and ancient ones preserved in the stratigraphic record. It brings together case studies from a range of continents, climatic and tectonic settings, some introducing innovative monitoring and analysis techniques, and it provides an overview of current debates in the field. This volume will be of particular interest to geologists, geomorphologists, sedimentologists and the general reader with an interest in Earth science.

Description / Table of Contents: Abstract The Himalaya mountains contain not only one of the largest concentrations of ice outside the polar regions, but contribute to the hydrological requirements of large populations spread over seven nations. The exceptionally high elevations of this low-latitude cryosphere presents a natural laboratory and archives to study climate–tectonics interactions as well as regional v. global climate influences. The existing base-level data on the Himalayan cryosphere are highly variable. Several climate fluctuations occurred during the late Quaternary (MIS1–MIS5, especially the last c. 100 ka), which led to the evolution of the Himalayan landscape. Detailed studies of these archives, along with those of the present cryosphere and related hydrosphere, are essential for understanding the controls on present and future hydrology of the glacial-fed mountain rivers. This volume, a follow-up of the XII International Symposium on Antarctic Earth Science, Goa (A SCAR symposium), provides new data from locales spread over the entire Himalaya region and from Tibet. It provides a glimpse of the late Quaternary cryosphere, as well as a discussion in the last section on sustainability in the context of geohazard mitigations as well as the hydrological budget.

Description / Table of Contents: Earth's climate varies continuously across space and time, but humankind has witnessed only a small snapshot of its entire history, and instrumentally documented it for a mere 200 years. Our knowledge of past climate changes is therefore almost exclusively based on indirect proxy data, i.e. on indicators which are sensitive to changes in climatic variables and stored in environmental archives. Extracting the data from these archives allows retrieval of the information from earlier times. Obtaining accurate proxy information is a key means to test model predictions of the past climate, and only after such validation can the models be used to reliably forecast future changes in our warming world. The polar ice sheets of Greenland and Antarctica are one major climate archive, which record information about local air temperatures by means of the isotopic composition of the water molecules embedded in the ice. However, this temperature proxy is, as any indirect climate data, not a perfect recorder of past climatic variations. Apart from local air temperatures, a multitude of other processes affect the mean and variability of the isotopic data, which hinders their direct interpretation in terms of climate variations. This applies especially to regions with little annual accumulation of snow, such as the Antarctic Plateau. While these areas in principle allow for the extraction of isotope records reaching far back in time, a strong corruption of the temperature signal originally encoded in the isotopic data of the snow is expected. This dissertation uses observational isotope data from Antarctica, focussing especially on the East Antarctic low-accumulation area around the Kohnen Station ice-core drilling site, together with statistical and physical methods, to improve our understanding of the spatial and temporal isotope variability across different scales, and thus to enhance the applicability of the proxy for estimating past temperature variability. The presented results lead to a quantitative explanation of the local-scale (1–500 m) spatial variability in the form of a statistical noise model, and reveal the main source of the temporal variability to be the mixture of a climatic seasonal cycle in temperature and the effect of diffusional smoothing acting on temporally uncorrelated noise. These findings put significant limits on the representativity of single isotope records in terms of local air temperature, and impact the interpretation of apparent cyclicalities in the records. Furthermore, to extend the analyses to larger scales, the timescale-dependency of observed Holocene isotope variability is studied. This offers a deeper understanding of the nature of the variations, and is crucial for unravelling the embedded true temperature variability over a wide range of timescales.

Description / Table of Contents: This volume brings together a number of papers from two workshops with the theme, ‘Rain, Rivers, Reservoirs’, which considered the dynamic changes to river systems as part of natural processes, particularly changing climatic conditions. Bringing researchers from two different locations to Brazil and the UK allowed scientists to contribute to and promote, ‘debate on current research…on how the planet works and how we can live sustainably on it’. This volume features a series of papers on the geoscience of modern and ancient rivers from across the world (Brazil, United States, Spain, Argentina, Canada, India and the UK), their evolution through time, their management, their deposits and their engineering, with both subsurface aquifers/hydrocarbon reservoirs (of Carboniferous, Triassic and Cretaceous age) and surface reservoirs considered.

Description / Table of Contents: This volume provides a synopsis of current research on volcanic processes, as gained through the use of palaeomagnetic and rock magnetic techniques. Thermoremanent magnetization information provides a powerful means of deciphering thermal processes in volcanic deposits, including estimating the emplacement temperature of pyroclastic deposits, which allows us to understand better the rates of cooling during eruption and transport. Anisotropy of magnetic susceptibility and anisotropy of remanence are used primarily to investigate rock fabrics and to quantify flow dynamics in dykes, lava flows, and pyroclastic deposits, as well as identify vent locations. Rock-magnetic characteristics allow correlation of volcanic deposits, but also provide means to date volcanic deposits and to understand better their cooling history. Because lava flows are typically good recorders of past magnetic fields, data from them allow understanding of changes in geomagnetic field directions and intensity, providing clues on the origin of Earth's magnetic field.

Description / Table of Contents: The Himalayan mountain belt, which developed during the India–Asia collision starting about 55 Ma ago, is a dramatically active orogen and it is regarded as the classic collisional orogen. It is characterized by an impressively continuous 2500 km of tectonic units, thrusts and normal faults, as well as large volumes of high-grade metamorphic rocks and granites exposed at the surface. This constitutes an invaluable field laboratory, where amazing crustal sections can be observed directly in very deep gorges. It is possible to unravel the tectonic and metamorphic evolution of litho-units, to observe the mechanisms of exhumation of deep-seated rocks and the propagation of the deformation. Himalayan tectonics has been the target of many studies from numerous international researchers over the years. In the last 15 years there has been an explosion of data and theories from both geological and geophysical perspectives. This book presents the results of integrated multidisciplinary studies, including geology, petrology, magmatism, geochemistry, geochronology and geophysics, of the structures and processes affecting the continental lithosphere. These processes and their spatial and temporal evolution have major consequences on the geometry and kinematics of the India–Eurasia collision zone.

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

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

Description / Table of Contents: Sea-level change has influenced human population globally since prehistoric times. Even in early phases of cultural development human populations were faced with marine regression and transgression as a result of changing climate and corresponding glacio-isostatic adjustment. Global marine regression during the last glaciation changed the palaeogeography of the continental shelf, converting former marine environments to attractive terrestrial habitats for prehistoric humans. These areas of the shelf were used as hunting and gathering areas, as migration routes between continents, and most probably witnessed the earliest developments in seafaring and marine exploitation, until the postglacial transgression re-submerged these palaeo-landscapes. Based on modern marine research technologies and the integration of large databases, proxy data are increasingly available for the reconstruction of Quaternary submerged landscapes. Also, prehistoric archaeological remains from the recent sea bottom are shedding new light on human prehistoric development driven by rapidly changing climate and environment. This publication contributes to the exchange of ideas and new results in this young and challenging field of underwater palaeoenvironmental investigation.

Description / Table of Contents: The continental crust is our archive of Earth history, and the store of many natural resources; however, many key questions about its formation and evolution remain debated and unresolved: - What processes are involved in the formation, differentiation and evolution of continental crust, and how have these changed throughout Earth history? - How are plate tectonics, the supercontinent cycle and mantle cooling linked with crustal evolution? - What are the rates of generation and destruction of the continental crust through time? - How representative is the preserved geological record? A range of approaches are used to address these questions, including field-based studies, petrology and geochemistry, geophysical methods, palaeomagnetism, whole-rock and accessory-phase isotope chemistry and geochronology. Case studies range from the Eoarchaean to Phanerozoic, and cover many different cratons and orogenic belts from across the continents.

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

Description / Table of Contents: Corentin Caudron, Takeshi Ohba, and Bruno Capaccioni: Geochemistry and geophysics of active volcanic lakes: an introduction / Geological Society, London, Special Publications, 437:1-8, first published on April 20, 2017, doi:10.1144/SP437.18 --- Acidic lakes --- Vincent van Hinsberg, Nathalie Vigouroux, Stephanie Palmer, Kim Berlo, Guillaume Mauri, Anthony Williams-Jones, Jeffrey Mckenzie, Glyn Williams-Jones, and Tobias Fischer: Element flux to the environment of the passively degassing crater lake-hosting Kawah Ijen volcano, Indonesia, and implications for estimates of the global volcanic flux / Geological Society, London, Special Publications, 437:9-34, first published on December 17, 2015, doi:10.1144/SP437.2 --- Hendra Gunawan, Corentin Caudron, John Pallister, Sofyan Primulyana, Bruce Christenson, Wendy Mccausland, Vincent van Hinsberg, Jennifer Lewicki, Dmitri Rouwet, Peter Kelly, Christoph Kern, Cynthia Werner, Jeffrey B. Johnson, Sri Budi Utami, Devy Kamil Syahbana, Ugan Saing, Suparjan, Bambang Heri Purwanto, Christine Sealing, Maria Martinez Cruz, Sukir Maryanto, Philipson Bani, Antoine Laurin, Agathe Schmid, Kyle Bradley, I Gusti Made Agung Nandaka, and Mochammad Hendrasto: New insights into Kawah Ijen's volcanic system from the wet volcano workshop experiment / Geological Society, London, Special Publications, 437:35-56, first published on February 25, 2016, doi:10.1144/SP437.7 --- Corentin Caudron, Guillaume Mauri, Glyn Williams-Jones, Thomas Lecocq, Devy Kamil Syahbana, Raphael De Plaen, Loic Peiffer, Alain Bernard, and Ginette Saracco: New insights into the Kawah Ijen hydrothermal system from geophysical data / Geological Society, London, Special Publications, 437:57-72, first published on January 22, 2016, doi:10.1144/SP437.4 --- Dmitri Rouwet, Raúl Mora-Amador, Carlos J. Ramírez-Umaña, Gino González, and Salvatore Inguaggiato: Dynamic fluid recycling at Laguna Caliente (Poás, Costa Rica) before and during the 2006–ongoing phreatic eruption cycle (2005–10) / Geological Society, London, Special Publications, 437:73-96, first published on March 24, 2016, doi:10.1144/SP437.11 --- B. Capaccioni, D. Rouwet, and F. Tassi: HCl degassing from extremely acidic crater lakes: preliminary results from experimental determinations and implications for geochemical monitoring / Geological Society, London, Special Publications, 437:97-106, first published on March 24, 2016, doi:10.1144/SP437.12 --- Mariano R. Agusto, Alberto Caselli, Romina Daga, Johan Varekamp, Alcira Trinelli, María Dos Santos Afonso, María Laura Velez, Pablo Euillades, and Sergio Ribeiro Guevara: The crater lake of Copahue volcano (Argentina): geochemical and thermal changes between 1995 and 2015 / Geological Society, London, Special Publications, 437:107-130, first published on December 23, 2016, doi:10.1144/SP437.16 --- Pedro A. Hernández, Gladys V. Melián, Luis Somoza, Mª Carmencita Arpa, Nemesio M. Pérez, Ericson Bariso, Hirochicka Sumino, Eleazar Padrón, Johan C. Varekamp, José Albert-Beltran, and Renato Solidum: The acid crater lake of Taal Volcano, Philippines: hydrogeochemical and hydroacoustic data related to the 2010–11 volcanic unrest / Geological Society, London, Special Publications, 437:131-152, first published on February 2, 2017, doi:10.1144/SP437.17 --- D. Rouwet and M. Iorio: The sedimentation of Suminagashi-like floating clay patterns at El Chichón crater lake (Chiapas, Mexico) / Geological Society, London, Special Publications, 437:153-161, first published on February 4, 2016, doi:10.1144/SP437.9 --- Neutral lakes --- Tomofumi Kozono, Minoru Kusakabe, Yutaka Yoshida, Romaric Ntchantcho, Takeshi Ohba, Gregory Tanyileke, and Joseph V. Hell: Numerical assessment of the potential for future limnic eruptions at lakes Nyos and Monoun, Cameroon, based on regular monitoring data / Geological Society, London, Special Publications, 437:163-175, first published on January 19, 2016, doi:10.1144/SP437.8 --- T. Ohba, S. Ooki, Y. Oginuma, M. Kusakabe, Y. Yoshida, A. Ueda, K. Anazawa, K. Saiki, K. Kaneko, Y. Miyabuchi, Issa, F. Aka, W. Fantong, A. Ako, G. Tanyileke, and J.V. Hell: Decreasing removal rate of the dissolved CO2 in Lake Nyos, Cameroon, after the installation of additional degassing pipes / Geological Society, London, Special Publications, 437:177-184, first published on December 23, 2015, doi:10.1144/SP437.6 --- Kazuto Saiki, Katsuya Kaneko, Takeshi Ohba, Mitsuhisa Sanemasa, Minoru Kusakabe, Romaric Ntchantcho, Alain Fouepe, Gregory Tanyileke, and Joseph V. Hell: Vertical distribution of dissolved CO2 in lakes Nyos and Monoun (Cameroon) as estimated by sound speed in water / Geological Society, London, Special Publications, 437:185-192, first published on February 18, 2016, doi:10.1144/SP437.10 --- Mitsuhisa Sanemasa, Kazuto Saiki, Katsuya Kaneko, Takeshi Ohba, Minoru Kusakabe, Romaric Ntchantcho, Alain Fouepe, Gregory Tanyileke, and Joseph V. Hell: A new method to determine dissolved CO2 concentration of lakes Nyos and Monoun using the sound speed and electrical conductivity of lake water / Geological Society, London, Special Publications, 437:193-203, first published on December 23, 2015, doi:10.1144/SP437.5 --- Yutaka Yoshida, Minoru Kusakabe, Issa, Takeshi Ohba, Gregory Tanyileke, and Joseph Victor Hell: Decreasing capability of the degassing systems at lakes Nyos and Monoun (Cameroon): a new gas removal system applied to Lake Monoun to prevent a future limnic eruption / Geological Society, London, Special Publications, 437:205-212, first published on December 17, 2015, doi:10.1144/SP437.3 --- Akiko Ozawa, Akira Ueda, Wilson Y. Fantong, Katsuro Anazawa, Yutaka Yoshida, Minoru Kusakabe, Takeshi Ohba, Greg Tanyileke, and Joseph V. Hell: Rate of siderite precipitation in Lake Nyos, Cameroon / Geological Society, London, Special Publications, 437:213-222, first published on June 22, 2016, doi:10.1144/SP437.13 --- Martin Zimmer, Franco Tassi, Orlando Vaselli, Christian Kujawa, Jacopo Cabassi, and Joerg Erzinger: The gas membrane sensor (GMS) method: a new analytical approach for real-time gas concentration measurements in volcanic lakes / Geological Society, London, Special Publications, 437:223-232, first published on December 17, 2015, doi:10.1144/SP437.1 --- Gladys Melián, Luís Somoza, Eleazar Padrón, Nemesio M. Pérez, Pedro A. Hernández, Hirochika Sumino, Victor H. Forjaz, and Zilda França: Surface CO2 emission and rising bubble plumes from degassing of crater lakes in São Miguel Island, Azores / Geological Society, London, Special Publications, 437:233-252, first published on August 12, 2016, doi:10.1144/SP437.14 --- J. N. Lefkowitz, J. C. Varekamp, R. W. Reynolds, and E. Thomas: A tale of two lakes: the Newberry Volcano twin crater lakes, Oregon, USA / Geological Society, London, Special Publications, 437:253-288, first published on November 25, 2016, doi:10.1144/SP437.15

Description / Table of Contents: Recent advances in karst research: from theory to fieldwork and applications / Mario Parise, Franci Gabrovsek, Georg Kaufmann and Natasa Ravbar / Geological Society, London, Special Publications, 466, 1-24, 3 May 2018, https://doi.org/10.1144/SP466.26 --- Karst geology, geomorphology, and speleogenesis --- Orogeny and the collapse of the Devonian Prairie Evaporite karst in Western Canada: impact on the overlying Cretaceous Athabasca Oil Sands / Paul L. Broughton / Geological Society, London, Special Publications, 466, 25-78, 8 November 2017, https://doi.org/10.1144/SP466.7 --- Tafoni and honeycomb structures as indicators of ascending fluid flow and hypogene karstification / Alexander Klimchouk / Geological Society, London, Special Publications, 466, 79-105, 28 November 2017, https://doi.org/10.1144/SP466.11 --- Relations between surface and underground karst forms inferred from terrestrial laser scanning / Aleksandar S. Petrović, Jelena Ćalić, Aleksandra Spalević and Marko Pantić / Geological Society, London, Special Publications, 466, 107-120, 31 January 2018, https://doi.org/10.1144/SP466.23 --- A genetic classification of caves and its application in eastern Austria / P. Oberender and L. Plan / Geological Society, London, Special Publications, 466, 121-136, 29 January 2018, https://doi.org/10.1144/SP466.21 --- Surface landforms and speleological investigation for a better understanding of karst hydrogeological processes: a history of research in southeastern Italy / M. Parise and L. Benedetto / Geological Society, London, Special Publications, 466, 137-153, 25 January 2018, https://doi.org/10.1144/SP466.25 --- The Puerto Princesa Underground River (Palawan, Philippines): some peculiar features of a tropical, high-energy coastal karst system / Giovanni Badino, Antonio De Vivo, Paolo Forti and Leonardo Piccini / Geological Society, London, Special Publications, 466, 155-170, 24 January 2018, https://doi.org/10.1144/SP466.22 --- Role of karst denudation on the accurate assessment of glacio-eustasy and tectonic uplift on carbonate coasts / John E. Mylroie and Joan R. Mylroie / Geological Society, London, Special Publications, 466, 171-185, 6 November 2017, https://doi.org/10.1144/SP466.2 --- Arid hypogene karst in a multi-aquifer system: hydrogeology and speleogenesis of Ashalim Cave, Negev Desert, Israel / Amos Frumkin and Boaz Langford / Geological Society, London, Special Publications, 466, 187-200, 6 November 2017, https://doi.org/10.1144/SP466.3 --- Pliocene–Pleistocene palaeoclimate reconstruction from Ashalim Cave speleothems, Negev Desert, Israel / Anton Vaks, Miryam Bar-Matthews, Avner Ayalon, Alan Matthews and Amos Frumkin / Geological Society, London, Special Publications, 466, 201-216, 15 December 2017, https://doi.org/10.1144/SP466.10 --- Karst hydrogeology --- Global distribution and use of water from karst aquifers / Zoran Stevanović / Geological Society, London, Special Publications, 466, 217-236, 4 January 2018, https://doi.org/10.1144/SP466.17 --- Characterization and hydraulic behaviour of the complex karst of the Kaibab Plateau and Grand Canyon National Park, USA / Casey J. R. Jones, Abraham E. Springer, Benjamin W. Tobin, Sarah J. Zappitello and Natalie A. Jones / Geological Society, London, Special Publications, 466, 237-260, 6 November 2017, https://doi.org/10.1144/SP466.5 --- Vulnerability assessment and its validation: the Gömör-Torna Karst, Hungary and Slovakia / Veronika Iván and Judit Mádl-Szőnyi / Geological Society, London, Special Publications, 466, 261-273, 29 November 2017, https://doi.org/10.1144/SP466.15 --- Hydrochemical and isotopic characterization of carbonate aquifers under natural flow conditions, Sierra Grazalema Natural Park, southern Spain / Damián Sánchez, Juan Antonio Barberá, Matías Mudarra, Bartolomé Andreo and José Francisco Martín / Geological Society, London, Special Publications, 466, 275-293, 28 November 2017, https://doi.org/10.1144/SP466.16 --- Climatological trends and anticipated karst spring quantity and quality: case study of the Slovene Istria / Nataša Ravbar, Gregor Kovačič, Metka Petrič, Janja Kogovšek, Clarissa Brun and Alenka Koželj / Geological Society, London, Special Publications, 466, 295-305, 6 December 2017, https://doi.org/10.1144/SP466.19 --- Preliminary analysis of the decrease in water level of Vrana Lake on the small carbonate island of Cres (Dinaric karst, Croatia) / Ognjen Bonacci / Geological Society, London, Special Publications, 466, 307-317, 6 November 2017, https://doi.org/10.1144/SP466.6 --- Karst modelling --- Numerical groundwater modelling in karst / Neven Kresic and Sorab Panday / Geological Society, London, Special Publications, 466, 319-330, 14 December 2017, https://doi.org/10.1144/SP466.12 --- Experiences in calibrating and evaluating lumped karst hydrological models / Andreas Hartmann / Geological Society, London, Special Publications, 466, 331-340, 6 December 2017, https://doi.org/10.1144/SP466.18 --- Geophysical observations and structural models of two shallow caves in gypsum/anhydrite-bearing rocks in Germany / Georg Kaufmann and Douchko Romanov / Geological Society, London, Special Publications, 466, 341-357, 6 December 2017, https://doi.org/10.1144/SP466.13 --- Models of temperature, entropy production and convective airflow in caves / Giovanni Badino / Geological Society, London, Special Publications, 466, 359-379, 31 January 2018, https://doi.org/10.1144/SP466.24 --- Karst hazards and management --- Evaluating the susceptibility to anthropogenic sinkholes in Apulian calcarenites, southern Italy / A. Fiore, N. L. Fazio, P. Lollino, M. Luisi, M. N. Miccoli, R. Pagliarulo, M. Perrotti, L. Pisano, L. Spalluto, C. Vennari, G. Vessia and M. Parise / Geological Society, London, Special Publications, 466, 381-396, 4 January 2018, https://doi.org/10.1144/SP466.20 --- Groundwater flood hazards and mechanisms in lowland karst terrains / Owen Naughton, Ted McCormack, Laurence Gill and Paul Johnston / Geological Society, London, Special Publications, 466, 397-410, 11 December 2017, https://doi.org/10.1144/SP466.9 --- Škocjan Caves, Slovenia: an integrative approach to the management of a World Heritage Site / Vanja Debevec, Borut Peric, Samo Šturm, Tomaž Zorman and Peter Jovanovič / Geological Society, London, Special Publications, 466, 411-429, 18 December 2017, https://doi.org/10.1144/SP466.14 --- Karst-specific composite model for informed resource management decisions on the Biosfera de la Reserva Selva el Ocote, Chiapas, Mexico / Johanna L. Kovarik and Philip E. van Beynen / Geological Society, London, Special Publications, 466, 431-442, 6 November 2017, https://doi.org/10.1144/SP466.1 --- A review and statistical assessment of the criteria for determining cave significance / Augusto S. Auler, Tatiana A. R. Souza, Daniela C. Sé and Gustavo A. Soares / Geological Society, London, Special Publications, 466, 443-459, 28 November 2017, https://doi.org/10.1144/SP466.8 --- What will be the future of the giant gypsum crystals of Naica mine? / Paolo Forti / Geological Society, London, Special Publications, 466, 461-475, 6 November 2017, https://doi.org/10.1144/SP466.4

Description / Table of Contents: Geohazards in Indonesia: Earth science for disaster risk reduction – introduction / Phil R. Cummins / Geological Society, London, Special Publications, 441, 1-7, 6 September 2017, https://doi.org/10.1144/SP441.11 --- Waves of destruction in the East Indies: the Wichmann catalogue of earthquakes and tsunami in the Indonesian region from 1538 to 1877 / Ron Harris and Jonathan Major / Geological Society, London, Special Publications, 441, 9-46, 24 May 2016, https://doi.org/10.1144/SP441.2 --- Assessing tsunami hazard using heterogeneous slip models in the Mentawai Islands, Indonesia / Jonathan D. Griffin, Ignatius R. Pranantyo, Widjo Kongko, Afif Haunan, Rahayu Robiana, Victoria Miller, Gareth Davies, Nick Horspool, Imun Maemunah, Wisnu B. Widjaja, Danny H. Natawidjaja and Hamzah Latief / Geological Society, London, Special Publications, 441, 47-70, 2 June 2016, https://doi.org/10.1144/SP441.3 --- Fault systems of the eastern Indonesian triple junction: evaluation of Quaternary activity and implications for seismic hazards / Ian M. Watkinson and Robert Hall / Geological Society, London, Special Publications, 441, 71-120, 19 December 2016, https://doi.org/10.1144/SP441.8 --- Sensitivity analysis for probabilistic seismic hazard analysis (PSHA) in the Aceh Fault Segment, Indonesia / Amalfi Omang, Phil R. Cummins, David Robinson and Sri Hidayati / Geological Society, London, Special Publications, 441, 121-131, 9 June 2016, https://doi.org/10.1144/SP441.5 --- A probabilistic seismic hazard assessment for Sulawesi, Indonesia / A. Cipta, R. Robiana, J. D. Griffin, N. Horspool, S. Hidayati and Phil R. Cummins / Geological Society, London, Special Publications, 441, 133-152, 26 April 2016, https://doi.org/10.1144/SP441.6 --- Development of an engineering bedrock map beneath Jakarta based on microtremor array measurements / M. Ridwan, S. Widiyantoro, M. Irsyam, Afnimar and H. Yamanaka / Geological Society, London, Special Publications, 441, 153-165, 28 July 2016, https://doi.org/10.1144/SP441.7 --- Towards real-time earthquake impact alerting in Indonesia / Sigit Pramono, Trevor I. Allen, Craig Bugden, Rakhindro Pandhu, Isabella Nindya, Hadi Ghasemi and Masturyono / Geological Society, London, Special Publications, 441, 167-178, 18 May 2016, https://doi.org/10.1144/SP441.4 --- Empirical fatality model for Indonesia based on a Bayesian approach / I. Wayan Sengara, Made Suarjana, M. Addifa Yulman, Hadi Gashemi and Hyeuk Ryu / Geological Society, London, Special Publications, 441, 179-187, 24 April 2017, https://doi.org/10.1144/SP441.9 --- Evaluating a volcanic ash ground-loading hazard at Gunung Ciremai, West Java, Indonesia using PF3D / A. N. Bear-Crozier, N. Kartadinata, A. Heriwaseso and O. Nielsen / Geological Society, London, Special Publications, 441, 189-198, 24 March 2016, https://doi.org/10.1144/SP441.1 --- Understanding the trigger for the LUSI mud volcano eruption from ground deformation signatures / Heri Andreas, Hasanuddin Z. Abidin, Teguh P. Sidiq, Irwan Gumilar, Yosuke Aoki, Agus L. Hakim and Prihadi Sumintadiredja / Geological Society, London, Special Publications, 441, 199-212, 10 July 2017, https://doi.org/10.1144/SP441.10

Description / Table of Contents: Geochemical applications in petroleum systems analysis: new constraints and the power of integration / M. Lawson, M. J. Formolo, L. Summa and J. M. Eiler / Geological Society, London, Special Publications, 468, 1-21, 19 February 2018, https://doi.org/10.1144/SP468.6 --- Source-rock identification and the temperature/timing of hydrocarbon generation --- The utility of methane clumped isotopes to constrain the origins of methane in natural gas accumulations / Daniel A. Stolper, Michael Lawson, Michael J. Formolo, Cara L. Davis, Peter M. J. Douglas and John M. Eiler / Geological Society, London, Special Publications, 468, 23-52, 14 December 2017, https://doi.org/10.1144/SP468.3 --- The isotopic structures of geological organic compounds / John M. Eiler, Matthieu Clog, Michael Lawson, Max Lloyd, Alison Piasecki, Camilo Ponton and Hao Xie / Geological Society, London, Special Publications, 468, 53-81, 14 December 2017, https://doi.org/10.1144/SP468.4 --- Vanadium isotope composition of crude oil: effects of source, maturation and biodegradation / Yongjun Gao, John F. Casey, Luis M. Bernardo, Weihang Yang and K. K. (Adry) Bissada / Geological Society, London, Special Publications, 468, 83-103, 14 December 2017, https://doi.org/10.1144/SP468.2 --- Carbon and hydrogen isotopic compositions of n-alkanes as a tool in petroleum exploration / Nikolai Pedentchouk and Courtney Turich / Geological Society, London, Special Publications, 468, 105-125, 14 December 2017, https://doi.org/10.1144/SP468.1 --- Mechanisms and time-scales associated with hydrocarbon migration, trapping, storage and alteration --- Noble gases in conventional and unconventional petroleum systems / David J. Byrne, P. H. Barry, M. Lawson and C. J. Ballentine / Geological Society, London, Special Publications, 468, 127-149, 14 December 2017, https://doi.org/10.1144/SP468.5 --- Differentiating between biogenic and thermogenic sources of natural gas in coalbed methane reservoirs from the Illinois Basin using noble gas and hydrocarbon geochemistry / Myles T. Moore, David S. Vinson, Colin J. Whyte, William K. Eymold, Talor B. Walsh and Thomas H. Darrah / Geological Society, London, Special Publications, 468, 151-188, 18 January 2018, https://doi.org/10.1144/SP468.8 --- The impact of fluid flow on reservoir properties --- Testing clumped isotopes as a reservoir characterization tool: a comparison with fluid inclusions in a dolomitized sedimentary carbonate reservoir buried to 2–4 km / John M. MacDonald, Cédric M. John and Jean-Pierre Girard / Geological Society, London, Special Publications, 468, 189-202, 14 December 2017, https://doi.org/10.1144/SP468.7

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