gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2017-8-3-0250gtcrust-391Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSGEOCHEMISTRY AND ORIGIN OF THE EASTERN SAYAN OPHIOLITES, TUVA-MONGOLIAN MICROCONTINENT (SOUTHERN SIBERIA)GEOCHEMISTRY AND ORIGIN OF THE EASTERN SAYAN OPHIOLITES, TUVA-MONGOLIAN MICROCONTINENT (SOUTHERN SIBERIA)BelyaevV. A.BelyaevV. A.

Taipei;

Irkutsk

Taipei;

Irkutsk

WangK.-L.WangK.-L.

Taipei

Taipei

GornovaM. A.GornovaM. A.

Irkutsk

Irkutsk

Dril’S. I.Dril’S. I.

Irkutsk

Irkutsk

KarimovA. A.KarimovA. A.

Irkutsk

Irkutsk

MedvedevA. Ya.MedvedevA. Ya.

Irkutsk

Irkutsk

NoskovaYu. V.NoskovaYu. V.

Irkutsk

Irkutsk

Institute of Earth Sciences, Academia Sinica; A.P. Vinogradov Institute of Geochemistry, Siberian Branch of RASТайваньInstitute of Earth Sciences, Academia Sinica; A.P. Vinogradov Institute of Geochemistry, Siberian Branch of RASTaiwan, Province of ChinaInstitute of Earth Sciences, Academia Sinica; Department of Geosciences, National Taiwan UniversityТайваньInstitute of Earth Sciences, Academia Sinica; Department of Geosciences, National Taiwan UniversityTaiwan, Province of ChinaA.P. Vinogradov Institute of Geochemistry, Siberian Branch of RASРоссияA.P. Vinogradov Institute of Geochemistry, Siberian Branch of RASRussian Federation20171010201783411415Copyright © Belyaev V.A., Wang K., Gornova M.A., Dril’ S.I., Karimov A.A., Medvedev A.Y., Noskova Y.V., 20172017Belyaev V.A., Wang K., Gornova M.A., Dril’ S.I., Karimov A.A., Medvedev A.Y., Noskova Y.V.Belyaev V.A., Wang K., Gornova M.A., Dril’ S.I., Karimov A.A., Medvedev A.Y., Noskova Y.V.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/391

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].

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].

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The authors declare that there are no conflicts of interest present.