Thomas Theunissen
The usual place Room 2G16c, 2nd floor, Realfabyyget, 41 Allégaten, Bergen, NorwayTopography 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 …