GEOLOGICAL STRUCTURE AND INDICATORS OF HYDROTHERMAL ORE-BEARING ACTIVITY AT THE JUNCTION OF THE SOUTHERN RIFT SEGMENT AND THE DOLDRUMS TRANSFORM FRACTURE ZONE, CENTRAL ATLANTIC

dc.contributor.author	Skolotnev S.G.
dc.contributor.author	Peive A.A.
dc.contributor.author	Lavrushin V.Yu.
dc.contributor.author	Eskin A.E.
dc.contributor.author	Petrova V.V.
dc.contributor.author	Turko N.N.
dc.contributor.author	Chaplygina N.L.
dc.contributor.author	Sharkov E.V.
dc.contributor.author	Demidova T.A.
dc.contributor.author	Abramov S.S.
dc.contributor.author	Tsukanov N.V.
dc.contributor.author	Krinov D.I.
dc.contributor.author	Razdolina N.V.
dc.date.accessioned	2024-11-02T11:07:47Z
dc.date.available	2024-11-02T11:07:47Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13522480
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 3, 361-365
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46343
dc.description.abstract	Numerous occurrences of present-day hydrothermal activity in the Mid-Atlantic Ridge (MAR) have been discovered to date. These discoveries and nonuniform distribution of high-temperature spring fields have raised the issue of the causes of origination of hydrothermal ore-bearing systems and the elaboration of prospective. These causes cannot be clarified without indepth investigations of geology, tectonics, and geodynamics of ore-bearing sites.
dc.title	GEOLOGICAL STRUCTURE AND INDICATORS OF HYDROTHERMAL ORE-BEARING ACTIVITY AT THE JUNCTION OF THE SOUTHERN RIFT SEGMENT AND THE DOLDRUMS TRANSFORM FRACTURE ZONE, CENTRAL ATLANTIC
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06030044

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