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

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dc.contributor.authorSkolotnev S.G.
dc.contributor.authorPeive A.A.
dc.contributor.authorLavrushin V.Yu.
dc.contributor.authorEskin A.E.
dc.contributor.authorPetrova V.V.
dc.contributor.authorTurko N.N.
dc.contributor.authorChaplygina N.L.
dc.contributor.authorSharkov E.V.
dc.contributor.authorDemidova T.A.
dc.contributor.authorAbramov S.S.
dc.contributor.authorTsukanov N.V.
dc.contributor.authorKrinov D.I.
dc.contributor.authorRazdolina N.V.
dc.date.accessioned2024-11-02T11:07:47Z
dc.date.available2024-11-02T11:07:47Z
dc.date.issued2006
dc.description.abstractNumerous 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.identifierhttps://www.elibrary.ru/item.asp?id=13522480
dc.identifier.citationDoklady Earth Sciences, 2006, 407, 3, 361-365
dc.identifier.doi10.1134/S1028334X06030044
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/46343
dc.titleGEOLOGICAL 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.typeСтатья

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