Sedimentology and depositional environment of the Kobbe and Steinkobbe formations in the Nordkapp Basin, Sentralbanken High and the Svalis Dome, Barents Sea
The Mesozoic succession in the Barents Sea was deposited in a relatively shallow epicontinental basin that gradually were infilled during the Triassic by north and north-west progradation of an extensive deltaic system mainly sourced from the Baltic Shield in the south and the Uralian Mountains and...
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Other Authors: | , |
Format: | Master Thesis |
Language: | English |
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NTNU
2018
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Online Access: | http://hdl.handle.net/11250/2563518 |