The Håkon Mosby mud volcano: 330 000 years of focused fluid flow activity at the SW Barents Sea slope
Studying the morphology and subsurface geometry of mud volcanoes provides insights into their activity. This paper describes the internal structure of the Håkon Mosby mud volcano (HMMV) in the southwestern Barents Sea and presents a conceptual model of its evolution. The lack of a mud edifice and th...
Published in: | Marine Geology |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
2009
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Subjects: | |
Online Access: | https://eprints.soton.ac.uk/66436/ |