gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2017-8-3-0252gtcrust-393Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSTECTONICS AND GEODYNAMICS OF THE ALTAI-JUNGGAR OROGEN IN THE VENDIAN-PALEOZOIC: IMPLICATIONS FOR THE CONTINENTAL EVOLUTION AND GROWTH OF THE CENTRAL ASIAN FOLD BELTTECTONICS AND GEODYNAMICS OF THE ALTAI-JUNGGAR OROGEN IN THE VENDIAN-PALEOZOIC: IMPLICATIONS FOR THE CONTINENTAL EVOLUTION AND GROWTH OF THE CENTRAL ASIAN FOLD BELTBuslovM. M.BuslovM. M.

Novosibirsk

Novosibirsk

CaiK.CaiK.

Urumqi 830011

Urumqi 830011

V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of RASРоссияV.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of RASRussian FederationXinjiang Research Centre for Mineral Resources, Xinjiang Institute of Ecology and Geography, Chinese Academy of SciencesКитайXinjiang Research Centre for Mineral Resources, Xinjiang Institute of Ecology and Geography, Chinese Academy of SciencesChina20171010201783421427Copyright © Buslov M.M., Cai K., 20172017Buslov M.M., Cai K.Buslov M.M., Cai K.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/393

In the end of the 20th century folded structures of central Asia were regarded as formed by accretion and collision of the Paleo-Asian oceanic plate and Siberia continent.

In the end of the 20th century folded structures of central Asia were regarded as formed by accretion and collision of the Paleo-Asian oceanic plate and Siberia continent.

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