Focused fluid flow through the gas-hydrate stability zone on the Vestnesa Ridge, offshore W-svalbard
Abstract: Numerous unburied seafloor pockmarks are related to current methane-leakage at Vestnesa Ridge (~79° N), west of Svalbard. About 50 km long and 1-3 km wide, Vestnesa Ridge is a 1-2 km thick sediment drift to the north of the active Molloy transform – on the eastern spreading segment. With i...
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Format: | Master Thesis |
Language: | English |
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UiT The Arctic University of Norway
2014
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Online Access: | https://hdl.handle.net/10037/6507 |