GEOCHEMICAL ACTIVITY OF FAULTS IN THE BAIKAL RIFT ZONE (MERCURY, RADON, AND THORON)

dc.contributor.authorKoval P.V.
dc.contributor.authorUdodo Yu.N.
dc.contributor.authorYasenovskii A.A.
dc.contributor.authorAndrulaitis L.D.
dc.contributor.authorSan'kov V.A.
dc.date.accessioned2024-11-02T11:07:57Z
dc.date.available2024-11-02T11:07:57Z
dc.date.issued2006
dc.description.abstractGeochemically active faults are accompanied by emission of matter into the host rocks and atmosphere. In particular, they include active faults of volcanic and rift zones accompanied by elevated heat flow, volcanism, thermal springs, and gas emission. A part of the emitted components (in particular, Hg, S, trace elements, and others) is a priori considered juvenile products.
dc.identifierhttps://www.elibrary.ru/item.asp?id=13524316
dc.identifier.citationDoklady Earth Sciences, 2006, 409, 6, 912-915
dc.identifier.doi10.1134/S1028334X06060171
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/46380
dc.titleGEOCHEMICAL ACTIVITY OF FAULTS IN THE BAIKAL RIFT ZONE (MERCURY, RADON, AND THORON)
dc.typeСтатья

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