Geological perspectives of the East Greenland continental margin
The East Greenland continental margin can be divided into a northern area showing evidence for plate separation and sutiuing of Hudsonian, Grenvillian and Caledonian ages followed by post-Late Caledonian molasse sedimentation and Mesozoic rifting, and a southern area which apparently formed a craton...
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.464.8649 http://2dgf.dk/xpdf/bull29-01-02-77-101.pdf |