Abstract
The southern Norwegian Barents Sea and the Northeast Greenland shelf are conjugate margins that formed a contiguous salt basin during the Pennsylvanian to Early Permian. Modern seismic data and cross-section restoration are used to evaluate three aspects of the salt tectonics: the relationship between evaporite deposition and rifting; the nature of the Gipsdalen Group layered evaporite sequence (LES); and the origin and evolution of salt-related deformation.
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Schedule a callMore From: Permo-Triassic Salt Provinces of Europe, North Africa and the Atlantic Margins
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