DEVONIAN-CARBONIFEROUS MAGMATISM AND METALLOGENY IN THE SOUTH URAL ACCRETIONARY-COLLISIONAL SYSTEM

The oceanic stage in the history of the South Urals completed in the Ordovician – Early Silurian. The Ordovician through Devonian events in the region included the formation of an island arc in the East Ural zone from the Middle Ordovician to Silurian; westward motion of the subduction zone in the L...

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Päätekijät: A. M. Kosarev, A. G. Vladimirov, A. I. Khanchuk, D. N. Salikhov, V. B. Kholodnov, T. A. Osipova, G. A. Kallistov, I. B. Seravkin, I. R. Rakhimov, G. T. Shafigullina
Aineistotyyppi: Artigo
Kieli:Inglês
Julkaistu: Institute of the Earth's crust, Siberian Branch of RAS 2021-06-01
Sarja:Geodinamika i Tektonofizika
Aiheet:
plate tectonics
plume tectonics
subduction
transform boundary
collision settings
island arc
magmatism
metallogeny
mineral deposit
urals
altai
Linkit:https://www.gt-crust.ru/jour/article/view/1216
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