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...
Published in: | GEUS Bulletin |
---|---|
Main Authors: | , , |
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 |