THE ERDENETUIN-OBO PORPHYRY CU-MO MAGMA CHAMBER (MONGOLIA) AS A REFLECTION OF THE PERMIAN-TRIASSIC SUPERPLUME

THE ERDENETUIN-OBO PORPHYRY CU-MO MAGMA CHAMBER (MONGOLIA) AS A REFLECTION OF THE PERMIAN-TRIASSIC SUPERPLUME

Berzina A.P.; Dobretsov N.L.; Sotnikov V.I.; Ponomarchuk V.A.
xmlui.dri2xhtml.METS-1.0.item-citation: Doklady Earth Sciences, 2004, 399, 9, 1311-1314
Date: 2004

Abstract:

Large-scale Permian-Triassic magmatism of northern and central Asia has been recently proved to be of plume origin. Based on these concepts, the present paper considers a possible relationship between the evolution of the Erdenetuin-Obo porphyry Cu-Mo magma chamber and the Siberian superplume.

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