Davis Strait and Ungava Fault Zone: First results from a recent geophysical survey

The Davis Strait is a bathymetric high that separates the southern Baffin Bay and the northern Labrador Sea. These basins are the result of Cretaceous and Paleogene rifting and seafloor spreading between the North American plate and Greenland. Being one of the main tectonic features of the Davis Str...

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Bibliographic Details
Main Authors: Ehrhardt, A., Gohl, Karsten, Neben, Sönke, Damm, V., Funck, T., Gerlings, J.
Format: Conference Object
Language:unknown
Published: 2008
Subjects:
Online Access:https://epic.awi.de/id/eprint/19777/
https://hdl.handle.net/10013/epic.31693