COMPOSITION OF ORE-BEARING FLUIDS IN THE DAL'NEGORSK BOROSILICATE DEPOSIT, RUSSIA

dc.contributor.author	Prokof'ev V.Yu.
dc.contributor.author	Dobrovol'skaya M.G.
dc.contributor.author	Reif F.G.
dc.contributor.author	Ishkov Yu.M.
dc.contributor.author	Zhukova T.B.
dc.date.accessioned	2022-01-15T07:43:07Z
dc.date.available	2022-01-15T07:43:07Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13441695
dc.identifier.citation	Doklady Earth Sciences, 2003, 391, 5, 699-702
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34336
dc.description.abstract	The Dal’negorsk borosilicate deposit in Primorye is the typical economic-grade calcic-skarn boron deposit [1, 2]. The large-scale mineralization is restricted to the skarnized limestones of the Upper Triassic Tetyukha Formation. The skarn zone is 3.5 km long and 500 m thick. One can distinguish the skarn (wollastonite, hedenbergite, and andradite), borosilicate (danburite, axinite, datolite, and quartz), and quartz–carbonate (quartz, calcite, apophyllite, and ﬂuorite) stages of mineralization [1].
dc.title	COMPOSITION OF ORE-BEARING FLUIDS IN THE DAL'NEGORSK BOROSILICATE DEPOSIT, RUSSIA
dc.type	Статья

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