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

dc.contributor.author	Koval P.V.
dc.contributor.author	Udodo Yu.N.
dc.contributor.author	Yasenovskii A.A.
dc.contributor.author	Andrulaitis L.D.
dc.contributor.author	San'kov V.A.
dc.date.accessioned	2024-11-02T11:07:57Z
dc.date.available	2024-11-02T11:07:57Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13524316
dc.identifier.citation	Doklady Earth Sciences, 2006, 409, 6, 912-915
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46380
dc.description.abstract	Geochemically 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.title	GEOCHEMICAL ACTIVITY OF FAULTS IN THE BAIKAL RIFT ZONE (MERCURY, RADON, AND THORON)
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06060171

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