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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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Auteurs principaux: 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
Langue:Inglês
Publié: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2021-06-01
Collection:Геодинамика и тектонофизика
Sujets:
ural orogen
granitoids
rifting
subduction
collision
plumes
anatexis
source
isotopic age
geochemistry
Accès en ligne:https://www.gt-crust.ru/jour/article/view/1208
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