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Distribution and abundance of gas hydrates in near‐surface deposits of the Håkon Mosby Mud Volcano, SW Barents Sea

The occurrence of gas hydrates at submarine mud volcanoes (MVs) located within the gas hydrate stability zone (GHSZ) is controlled by upward fluid and heat flux associated with MV activity. Determining the spatial distribution of gas hydrates at MVs is crucial to evaluate their sensitivity to known...

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Библиографические подробности
Главные авторы: Thomas Pape, Tomas Feseker, Sabine Kasten, David Fischer, Gerhard Bohrmann
Формат: Artigo
Язык:Inglês
Опубликовано: Wiley 2011-09-01
Серии:Geochemistry, Geophysics, Geosystems
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Online-ссылка:https://doi.org/10.1029/2011GC003575
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