A constellation of mud volcanoes originated from a buried Arctic mega-slide, Southwestern Barents Sea
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A constellation of mud volcanoes in the southwestern Barents Sea is reported to have originated from a buried Arctic mega-slide. Research on submarine mud volcanoes has been conducted in various locations, including the Taiwan accretionary prism. Studies have examined the discharge of fluids and sediment movement associated with mud volcanism, including the eruption of deep-sea mud volcanoes.
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