GEOCHEMISTRY AND ORIGIN OF THE EASTERN SAYAN OPHIOLITES, TUVA-MONGOLIAN MICROCONTINENT (SOUTHERN SIBERIA)

V. A. Belyaev; K.-L. Wang; M. A. Gornova; S. I. Dril’; A. A. Karimov; A. Ya. Medvedev; Yu. V. Noskova

doi:10.5800/GT-2017-8-3-0250

Геодинамика и тектонофизика (Sep 2017)

GEOCHEMISTRY AND ORIGIN OF THE EASTERN SAYAN OPHIOLITES, TUVA-MONGOLIAN MICROCONTINENT (SOUTHERN SIBERIA)

V. A. Belyaev,
K.-L. Wang,
M. A. Gornova,
S. I. Dril’,
A. A. Karimov,
A. Ya. Medvedev,
Yu. V. Noskova

Affiliations

V. A. Belyaev: Institute of Earth Sciences, Academia Sinica; A.P. Vinogradov Institute of Geochemistry, Siberian Branch of RAS
K.-L. Wang: Institute of Earth Sciences, Academia Sinica; Department of Geosciences, National Taiwan University
M. A. Gornova: A.P. Vinogradov Institute of Geochemistry, Siberian Branch of RAS
S. I. Dril’: A.P. Vinogradov Institute of Geochemistry, Siberian Branch of RAS
A. A. Karimov: A.P. Vinogradov Institute of Geochemistry, Siberian Branch of RAS
A. Ya. Medvedev: A.P. Vinogradov Institute of Geochemistry, Siberian Branch of RAS
Yu. V. Noskova: A.P. Vinogradov Institute of Geochemistry, Siberian Branch of RAS

DOI: https://doi.org/10.5800/GT-2017-8-3-0250
Journal volume & issue: Vol. 8, no. 3
pp. 411 – 415

Abstract

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The Eastern Sayan ophiolites (1020 Ma) of the Tuva-Mongolian microcontinent are believed to be the most ancient ophiolite of the Central Asian Orogenic Belt [Khain et al., 2002].

Published in Геодинамика и тектонофизика

ISSN: 2078-502X (Online)
Publisher: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
Country of publisher: Russian Federation
LCC subjects: Science
Website: http://gt.crust.irk.ru/index.en.html

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