Luisa Zuluaga

The usual place Room 2G16c, 2nd floor, Realfabyyget, 41 Allégaten, Bergen, Norway

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 …

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Thomas Theunissen

The usual place Room 2G16c, 2nd floor, Realfabyyget, 41 Allégaten, Bergen, Norway

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 …

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Jhon Meyer Munoz Barrera

The usual place Room 2G16c, 2nd floor, Realfabyyget, 41 Allégaten, Bergen, Norway

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 …

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Isabel Edmundson

The usual place Room 2G16c, 2nd floor, Realfabyyget, 41 Allégaten, Bergen, Norway

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 …

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Haakon Fossen

The usual place Room 2G16c, 2nd floor, Realfabyyget, 41 Allégaten, Bergen, Norway

The Pan-African Araçuai-West Congo belt (Brazil/W Africa) and why it needs revision, with references to the Caledonides and Himalayas.

Bjørn Nyberg

The usual place Room 2G16c, 2nd floor, Realfabyyget, 41 Allégaten, Bergen, Norway

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 …

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Thilo Wrona

The usual place Room 2G16c, 2nd floor, Realfabyyget, 41 Allégaten, Bergen, Norway

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).

Bjørn Burr Nyberg

The usual place Room 2G16c, 2nd floor, Realfabyyget, 41 Allégaten, Bergen, Norway

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, …

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Atle Rotevatn

The usual place Room 2G16c, 2nd floor, Realfabyyget, 41 Allégaten, Bergen, Norway

How do normal faults grow? In this geolunch talk, Atle will tell us about how he and some of his  friends/co-authors decided to have a stab at figuring out how normal faults actually grow while he was on sabbatical in New …

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Thomas Thuesen

The usual place Room 2G16c, 2nd floor, Realfabyyget, 41 Allégaten, Bergen, Norway

Source-to-sink in a western Norwegian fjord: How does landslides, floods and grinding glaciers influence sediment supply in the Holocene? Thomas Thuesen, William Helland-Hansen, Christian Haug Eide, Haflidi Haflidason, Atle Nesje   Western Norwegian fjord-valley systems represent archives of changes in …

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