Paleoceanography and Chronostratigraphy of two forthcoming ocean basins during the Upper Quaternary: The Red Sea and Corinth Rifts. Spyros present ongoing work from his PhD (Red Sea) as well as introduce future work related to the IODP expedition 381 (Corinth). …
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Status of geothermal research in Europe and beyond: updates from the 6th European Geothermal Workshop in Strasbourg Luisa was at the 6th European Geothermal Workshop in Strasbourg last week (10-11 October 2018). She will give us feedbacks about it. What …
Topography and subsidence during rifting. Thomas will give us updates about his ongoing work. Sedimentary basins result from the interlinked evolution of drainage area and uplift/subsidence of the continental domain (onshore and offshore). In this presentation, we will discuss the different causes that …
Structural configuration of the southern Klakk Fault Complex, mid-Norway. Crustal-scale fault geometry and interaction in basement rift shoulders. The thinning of continental crust from ~ 30 km to ~ 10 km characterises the necking domain of passive margins. In …
Elucidating key controls on column heights across the Snøhvit gas field, Hammerfest Basin, SW Barents Sea Izzy Edmundson, Atle Rotevatn, Roy Davies, Kjetil Broberg and Graham Yielding Faults can act as pathways or barriers to fluid flow and so …
The Pan-African Araçuai-West Congo belt (Brazil/W Africa) and why it needs revision, with references to the Caledonides and Himalayas.
NetworkGT: A GIS tool for Geometric and Topological Analysis of two-dimensional Fracture Networks Björn Nyberg, Casey Nixon Dimensions, arrangements, and interactions of individual fractures form fracture networks that control the mechanical and fluid flow properties of rock masses. Here …
The Dolomite Problem (i.e. the question of how the large quantities of dolomite observed in the geological record formed in the absence of equivalent modern environments).
Evolution of sedimentary systems with human activity Society develops in response to sedimentary systems. At the same time these systems are increasingly modified by society. For example, management of hydrological systems to meet water resource demands (e.g., dams, canals, weirs, …