Principal component analysis of seismic facies Thilo Wrona Seismic facies analyses are fundamental to the study of sedimentary, tectonic and magmatic systems using seismic reflection data. These analyses generally assume that seismic facies are: (1) well defined, (2) distinct and …
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What we have discovered in outer-rise – trench - volcanic arc systems: results from JAMSTEC’s marine geophysical studies Shuichi Kodaira, JAMSTEC - Kodaira_CV_2018_2pages Recent advancement of observational, experimental and theoretical studies of seismogenic zones have allowed us to develop a …
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.