THE LATE ORDOVICIAN AGE OF CAMPTONITES FROM THE AGARDAG COMPLEX OF SOUTHEASTERN TUVA AS AN INDICATOR OF THE PLUME-RELATED MAGMATISM DURING COLLISION PROCESSES

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dc.contributor.authorIzokh A.E.
dc.contributor.authorPolyakov G.V.
dc.contributor.authorMal'kovets V.G.
dc.contributor.authorShelepaev R.A.
dc.contributor.authorTravin A.V.
dc.contributor.authorLitasov Yu.D.
dc.contributor.authorGibsher A.A.
dc.date.accessioned2021-02-18T10:31:39Z
dc.date.available2021-02-18T10:31:39Z
dc.date.issued2001
dc.identifierhttps://elibrary.ru/item.asp?id=13371225
dc.identifier.citationDoklady Earth Sciences, 2001, 379, С. 5, 511-514
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/25095
dc.subjectOrdovicianen
dc.subject.agePaleozoic::Ordovicianen
dc.titleTHE LATE ORDOVICIAN AGE OF CAMPTONITES FROM THE AGARDAG COMPLEX OF SOUTHEASTERN TUVA AS AN INDICATOR OF THE PLUME-RELATED MAGMATISM DURING COLLISION PROCESSES
dc.typeСтатья

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