Time-lapse seismic analysis of focused fluid flow on the Vestnesa Ridge
The Vestnesa Ridge is a large sediment drift at water depths of 1200-1300 meter and is the northernmost known gas hydrate province that exists along the Arctic continental margin. Several pockmarks connected to vertical fluid flow features are present at the crest of the Vestnesa Ridge. The fluid fl...
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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/10037/9419 |