TRACE ELEMENT DISTRIBUTION IN THE KIMBERLITE-BITUMEN AND BASALT-BITUMEN SYSTEMS IN DIATREMES OF THE SIBERIAN CRATON

dc.contributor.author	Gottikh R.P.
dc.contributor.author	Pisotskii B.I.
dc.contributor.author	Zhuravlev D.Z.
dc.date.accessioned	2022-07-20T06:12:22Z
dc.date.available	2022-07-20T06:12:22Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13458839
dc.identifier.citation	Doklady Earth Sciences, 2004, 399, 9, 1222-1226
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38323
dc.description.abstract	The present paper considers trace element distribution in two natural systems: kimberlite-bitumen and basalt-bitumen. In the given case, carbonaceous matter in magmatic rocks is interpreted as a result of abiogenic synthesis from fluid components of melts at the final magmatic (pneumatolytic-hydrothermal) stages.
dc.title	TRACE ELEMENT DISTRIBUTION IN THE KIMBERLITE-BITUMEN AND BASALT-BITUMEN SYSTEMS IN DIATREMES OF THE SIBERIAN CRATON
dc.type	Статья

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