ОСОБЕННОСТИ СОСТАВА ОТЛОЖЕНИЙ ГРЯЗЕВОГО ВУЛКАНА ХААКОН МОСБИ (ЮГО-ЗАПАДНАЯ ЧАСТЬ БАРЕНЦЕВА МОРЯ)

dc.contributor.author	Крупская В.В.
dc.contributor.author	Андреева И.А.
dc.contributor.author	Сергеева Э.И.
dc.contributor.author	Черкашёв Г.А.
dc.date.accessioned	2021-08-03T04:33:39Z
dc.date.available	2021-08-03T04:33:39Z
dc.date.issued	2002
dc.identifier	https://www.elibrary.ru/item.asp?id=26803882
dc.identifier.citation	Литология и полезные ископаемые, 2002, , 2, 152-159
dc.identifier.issn	0024-497X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/30020
dc.description.abstract	The submarine Haakon Mosby mud volcano was studied in detail during several cruises, resulting in the collection of an abundant and diverse lithological material. Comprehensive field and laboratory studies made it possible to identify different types of sediments with specific granulometric and pelite fraction (<0.005 mm) compositions, as well as the regularity of their spatial distribution relative to various morphostructural zones of the mud volcano.
dc.title	ОСОБЕННОСТИ СОСТАВА ОТЛОЖЕНИЙ ГРЯЗЕВОГО ВУЛКАНА ХААКОН МОСБИ (ЮГО-ЗАПАДНАЯ ЧАСТЬ БАРЕНЦЕВА МОРЯ)
dc.type	Статья

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