Crustal structure of northwestern Svalbard and the adjacent Yermak Plateau: Evidence for Oligocene simple shear rifting and non-volcanic break-up.
In 1999 new seismic refraction data were collected off northwestern Svalbard and theadjacent Yermak Plateau. A 260 km long profile provides detailed velocity informationfor the northeastern edge of the Eurasian Continent and the adjacent Yermak Plateau.North of Forlandsundet Graben the depth of the...
| Main Authors: | , |
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| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
2003
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| Subjects: | |
| Online Access: | https://epic.awi.de/id/eprint/5248/ https://hdl.handle.net/10013/epic.15816 |