Department
Evolution and deformation of Forlandsundet Basin, Svalbard
Early Cretaceous sedimentation and Tertiary deformation if the Braents Shelf in north-central Spitsbergen: Bohemanflya, Isfjorden, Svalbard
Tectonically vesus climatically driven Cenozoic exhumation of the Eurasian plate margin, Svalbard: fission-track analyses.
Syn-glacial rebound and origin of fjords: Intraplate mountain belts and isostatic uplift due to surface processes.
Department of Earth Sciences
OrganizationUniversity of Minnesota
Emailklein004@umn.edu
Location
Minneapolis , Minnesota 55455
United StatesScience Specialties
geology, tectonics and sedimentary basin analysis, sedimentology, geodynamics, structural geologyCurrent Research
Oblique rifting in Svalbard and the Late Eocene-Oligocene demise of Laurasia with inception of Molloy RidgeEvolution and deformation of Forlandsundet Basin, Svalbard
Early Cretaceous sedimentation and Tertiary deformation if the Braents Shelf in north-central Spitsbergen: Bohemanflya, Isfjorden, Svalbard
Tectonically vesus climatically driven Cenozoic exhumation of the Eurasian plate margin, Svalbard: fission-track analyses.
Syn-glacial rebound and origin of fjords: Intraplate mountain belts and isostatic uplift due to surface processes.