PALEOZOIC GRANITOID MAGMATISM OF THE URALS: THE REFLECTION OF THE STAGES OF THE GEODYNAMIC AND GEOCHEMICAL EVOLUTION OF A COLLISIONAL OROGEN

The Ural mobile belt is an intracontinental epioceanic orogen that has already gone through all stages of the geodynamic development. Igneous rocks formed during each stage are important indicators for understanding the evolution of this belt and determining potential ore contents of its segments. W...

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Bibliographic Details
Main Authors: V. V. Kholodnov, G. Yu. Shardakova, V. N. Puchkov, G. A. Petrov, E. S. Shagalov, D. N. Salikhov, A. V. Korovko, S. V. Pribavkin, I. R. Rakhimov, N. S. Borodina
Format: Artigo
Language:Inglês
Published: Institute of the Earth's crust, Siberian Branch of RAS 2021-06-01
Series:Geodinamika i Tektonofizika
Subjects:
ural orogen
granitoids
rifting
subduction
collision
plumes
anatexis
source
isotopic age
geochemistry
Online Access:https://www.gt-crust.ru/jour/article/view/1208
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