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...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Geological Survey of Denmark and Greenland
2021-04-01
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| Series: | GEUS Bulletin |
| Subjects: | |
| Online Access: | https://geusbulletin.org/index.php/geusb/article/view/5298/12397 |