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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Autori principali:	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
Natura:	Artigo
Lingua:	Inglês
Pubblicazione:	Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2021-06-01
Serie:	Геодинамика и тектонофизика
Soggetti:	ural orogen granitoids rifting subduction collision plumes anatexis source isotopic age geochemistry
Accesso online:	https://www.gt-crust.ru/jour/article/view/1208
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