Mineralogy, Geochemistry, and Geochronology of the Yehe-Shigna Ophiolitic Massif, Tuva-Mongolian Microcontinent, Southern Siberia: Evidence for a Back-Arc Origin and Geodynamic Implications

Mineralogy, Geochemistry, and Geochronology of the Yehe-Shigna Ophiolitic Massif, Tuva-Mongolian Microcontinent, Southern Siberia: Evidence for a Back-Arc Origin and Geodynamic Implications

The new results have been represented of mineralogical–geochemical and geochronological studies of rocks of the Yehe-Shigna ophiolite massif located in the Tuva-Mongolian microcontinent in the northern part of the Central Asian orogenic belt (Eastern Sayan, Southern Siberia). The Yehe-Shigna ophioli...

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Bibliographic Details
Main Authors: Sergey Mikhailovich Zhmodik, Mikhail Mikhailovich Buslov, Bulat Batuevich Damdinov, Anatoli Georgievich Mironov, Valentin Borisovich Khubanov, Molon Gimitovich Buyantuyev, Ludmila Borisovna Damdinova, Evgeniya Vladimirovna Airiyants, Olga Nikolaevna Kiseleva, Dmitriy Konstantinovich Belyanin
Format: Article
Language:English
Published: MDPI AG 2022-03-01
Series:Minerals
Subjects:
Tuva-Mongolian microcontinent
Central-Asian orogenic belt
Gondwana supercontinent
ophiolites
mineralogy
geochemistry
Online Access:https://www.mdpi.com/2075-163X/12/4/390

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https://www.mdpi.com/2075-163X/12/4/390

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