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...
Main Authors: | , , , , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2008
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/19777/ https://hdl.handle.net/10013/epic.31693 |