GAS-HYDRATE ACCUMULATIONS OF SUBMARINE MUD-VOLCANO TYPE

dc.contributor.author	Ginsburg G.D.
dc.contributor.author	Gramberg I.S.
dc.contributor.author	Guliyev I.S.
dc.contributor.author	Ivanov V.L.
dc.contributor.author	Solov'yev V.A.
dc.contributor.author	Guseynov R.A.
dc.contributor.author	Dadashev A.A.
dc.contributor.author	Krotov A.G.
dc.contributor.author	Murdov C.S.
dc.contributor.author	Telepnev Y.V.
dc.date.accessioned	2020-04-13T10:49:36Z
dc.date.available	2020-04-13T10:49:36Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30964742
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 300, 3, 60-62
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16649
dc.description.abstract	The finding of gas-hydrates in breccia from a submarine mud volcano in the South Caspian deep-sea basin served as the basis for predicting the presence here of gas-hydrate accumulations of a special submarine mud-volcano type. The results of special surveys run in the southern Caspian in the summer of 1986 from the R/V Elm confirm the correctness of identifying such accumulations and allow them to be described in first approximation. Gas hydrates were detected and studied in the deposits of a mud volcano, revealed by seismoacoustic profiling. There also is indirect evidence of their presence on the flanks of two other presumed volcanoes.
dc.title	GAS-HYDRATE ACCUMULATIONS OF SUBMARINE MUD-VOLCANO TYPE
dc.type	Статья

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