Seabed depressions in the Ingøydjupet Trough and their relation to buried canyons on the Loppa High, Barents Sea
Large seabed depressions in the Ingøydjupet Trough have previously been interpreted to be formed by sub-glacial melt-water. However, fluid migration and gas expulsion occur over large parts of the Barents Sea, which are frequently associated with seabed depressions. This thesis studies how the seabe...
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Format: | Master Thesis |
Language: | English |
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UiT The Arctic University of Norway
2016
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Online Access: | https://hdl.handle.net/10037/9421 |