Thermo-tectonic development of the Wandel Sea Basin, North Greenland

The Carboniferous–Palaeogene Wandel Sea Basin of eastern North Greenland (north of 80°N, east of 40°W) is an important piece in the puzzle of Arctic geology. It is particularly important for understanding how the Paleocene–Eocene convergence between Greenland, the Canadian Arctic and Svalbard relate...

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Bibliographic Details
Published in:GEUS Bulletin
Main Authors: Peter Japsen, Paul F. Green, James A. Chalmers
Format: Article in Journal/Newspaper
Language:English
Published: Geological Survey of Denmark and Greenland 2021
Subjects:
Online Access:https://doi.org/10.34194/geusb.v45.5298
https://doaj.org/article/1e4801a877f34ea68acaa1dd0d04e7ca