Geology Of The Country Around Ramsgate And Dover

The White Cliffs of Dover are probably the best known geological feature of the country around Ramsgate and Dover.

Excavations at Cliffs End Farm, Thanet, Kent, undertaken in 2004/5 uncovered a dense area of archaeological remains including Bronze Age barrows and enclosures, and a large prehistoric mortuary feature, as well as a small early 6th to late 7th century Anglo-Saxon inhumation cemetery. An extraordinary series of human and animal remains were recovered from the Late Bronze Age–Middle Iron Age mortuary feature, revealing a wealth of evidence for mortuary rites including exposure, excarnation and curation. The site seems to have been largely abandoned in the later Iron Age and very little Romano-British activity was identified. In the early 6th century a small inhumation cemetery was established. Very little human bone survived within the 21 graves, where the burial environment differed from that within the prehistoric mortuary feature, but grave goods indicate ‘females’ and ‘males’ were buried here. Richly furnished graves included that of a ‘female’ buried with a necklace, a pair of brooches and a purse, as well as a ‘male’ with a shield covering his face, a knife and spearhead. In the Middle Saxon period lines of pits, possibly delineating boundaries, were dug, some of which contained large deposits of marine shells. English Heritage funded an extensive programme of radiocarbon and isotope analyses, which have produced some surprising results that shed new light on long distance contacts, mobility and mortuary rites during later prehistory. This volume presents the results of the investigations together with the scientific analyses, human bone, artefact and environmental reports.

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.

This book presents and describes an innovative method to simulate the growth of natural fractural networks in different geological environments, based on their geological history and fundamental geomechanical principles. The book develops techniques to simulate the growth and interaction of large populations of layer-bound fracture directly, based on linear elastic fracture mechanics and subcritical propagation theory. It demonstrates how to use these techniques to model the nucleation, propagation and interaction of layer-bound fractures in different orientations around large scale geological structures, based on the geological history of the structures. It also explains how to use these techniques to build more accurate discrete fracture network (DFN) models at a reasonable computational cost. These models can explain many of the properties of natural fracture networks observed in outcrops, using actual outcrop examples. Finally, the book demonstrates how it can be incorporated into flow modelling workflows using subsurface examples from the hydrocarbon and geothermal industries. Modelling the Evolution of Natural Fracture Networks will be of interest to anyone curious about understanding and predicting the evolution of complex natural fracture networks across large geological structures. It will be helpful to those modelling fluid flow through fractures, or the geomechanical impact of fracture networks, in the hydrocarbon, geothermal, CO2 sequestration, groundwater and engineering industries.

This Special Report comprehensively describes the stratigraphy and correlation of the Tertiary (Paleogene–Neogene) rocks of NW Europe and the adjacent Atlantic Ocean and is the summation of fifty years of research on Tertiary sediments by Chris King. His book is essential reading for all geologists who deal with Tertiary rocks across NW Europe, including those in the petroleum industry and geotechnical services as well as academic stratigraphers and palaeontologists. Introductory sections on chronostratigraphy, biostratigraphy and other methods of dating and correlation are followed by a regional summary of Tertiary sedimentary basins and their framework and an introduction to Tertiary igneous rocks. The third and largest segment comprises the regional stratigraphic summaries. Regions covered are the North Sea Basin, onshore areas of southern England and the eastern English Channel area, the North Atlantic margins (including non-marine basins in the Irish Sea and elsewhere) and the Paleogene igneous rocks of Scotland.