Basin modelling of the south-west Barents Sea
The south-west Barents Sea is an epicontinental platform consisting of N- to NNE-oriented basins separated by basement highs. It is underlain by thick sequences of Upper Paleozoic to Cenozoic sediments and Caledonian metamorphosed basement. The basins were formed during four distinct rift-phases in...
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Format: | Master Thesis |
Language: | English |
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2014
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Online Access: | http://hdl.handle.net/10852/43087 http://urn.nb.no/URN:NBN:no-47441 |