The Regional Methamorphism, Volcanism and Metallogeny
Vladimir Gugushvili
Broschiertes Buch

The Regional Methamorphism, Volcanism and Metallogeny

at the Eurasian Continental Margin Controlled by Geodynamic Regime of Phanerozoic Subduction and Collision of Tethys

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Subduction to collision evolution of the Tethys ocean is marked as distinct relation with the regional metamorphism, volcanism, hydrothermal alteration and metallogeny related to the western segment of the Eurasian active margin metallogenic belt. Regional metamorphism and formation of granite-metamorphic complexes are related to the first stage of subduction occurs before steepening of subducting slab. Further increasing of temperature and andesite melt fusion led to transition to island arc-calc-alkaline volcanism coincided with gold-copper-base metal mineralization. The steepening of subduc...