Umut Isikalp
Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen4D Evolution of a Salt Wall and Implication for Flanking Minibasin Stratigraphy: An Example from the Egersund Basin, Norwegian North Sea Umut Isikalp Salt diapirs are the most common type of salt-tectonic structure, occurring in many, if not all, salt …