Supplementary files for: Thermo-tectonic development of the Wandel Sea Basin, North Greenland
The Carboniferous–Palaeogene Wandel Sea Basin of eastern North Greenland (north of 80⁰N, east of 40⁰W) 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: | Dataset |
| Language: | unknown |
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GEUS Dataverse
2021
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| Subjects: | |
| Online Access: | https://dx.doi.org/10.22008/fk2/vlo6nq https://dataverse01.geus.dk/citation?persistentId=doi:10.22008/FK2/VLO6NQ |