A sedimentological study of the deltaic De Geerdalen Formation in Fulmardalen and of fluvial deposits in the Snadd Formation on the Finnmark Platform
In the Late Paleozoic, Svalbard and the Barents Sea were part of a large, shallow embayment located at the north-western corner of the supercontinent Pangea. During the Triassic this embayment was gradually filled with erosional products from the UralianMountains located in south-east. A large delta...
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| Other Authors: | , |
| Format: | Master Thesis |
| Language: | English |
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NTNU
2017
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| Online Access: | http://hdl.handle.net/11250/2444276 |