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

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

Izokh A.E.; Polyakov G.V.; Mal'kovets V.G.; Shelepaev R.A.; Travin A.V.; Litasov Yu.D.; Gibsher A.A.
xmlui.dri2xhtml.METS-1.0.item-citation: Doklady Earth Sciences, 2001, 379, С. 5, 511-514
Date: 2001

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