METALLOGENIC PROVINCE DERIVED FROM MANTLE SOURCES: ND, SR, S AND PB ISOTOPE EVIDENCE FROM THE CENTRAL ASIAN OROGENIC BELT

dc.contributor.author	Hong D.
dc.contributor.author	Zhang J.
dc.contributor.author	Wang T.
dc.contributor.author	Wang S.
dc.contributor.author	Xie X.
dc.date.accessioned	2022-02-03T04:39:25Z
dc.date.available	2022-02-03T04:39:25Z
dc.date.issued	2003
dc.identifier	https://elibrary.ru/item.asp?id=13727493
dc.identifier.citation	Gondwana Research, 2003, 6, 4, 711-728
dc.identifier.issn	1342-937X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34888
dc.description.abstract	The Central Asian Orogenic Belt (CAOB) is one of the most important regions for Cu, Au and polymetallic and rare metallic (Li, Be, Nb, Ta) mineralization over the world. Most of the ore deposits in the CAOB are closely associated with granitoids. Available Sr, Nd, S and Pb isotopic data indicate that the metallogenic epoch and sources of the mineral deposits in the CAOB are consistent with that of the regional granites. Available data suggest that mantle sources could have played an important role in the Paleozoic to Mesozoic mineralization in the CAOB.
dc.subject	Central Asian Orogenic Belt
dc.subject	metallogenic province
dc.subject	mantle source
dc.subject	Sr
dc.subject	Nd
dc.subject	S and Pb isotopes
dc.title	METALLOGENIC PROVINCE DERIVED FROM MANTLE SOURCES: ND, SR, S AND PB ISOTOPE EVIDENCE FROM THE CENTRAL ASIAN OROGENIC BELT
dc.type	Статья

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