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TECTONICS AND GEODYNAMICS OF THE ALTAI-JUNGGAR OROGEN IN THE VENDIAN-PALEOZOIC: IMPLICATIONS FOR THE CONTINENTAL EVOLUTION AND GROWTH OF THE CENTRAL ASIAN FOLD BELT

https://doi.org/10.5800/GT-2017-8-3-0252

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Аннотация

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.

Об авторах

M. M. Buslov
V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of RAS
Россия
Novosibirsk


K. Cai
Xinjiang Research Centre for Mineral Resources, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences
Китай
Urumqi 830011


Список литературы

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Для цитирования:


Buslov M.M., Cai K. TECTONICS AND GEODYNAMICS OF THE ALTAI-JUNGGAR OROGEN IN THE VENDIAN-PALEOZOIC: IMPLICATIONS FOR THE CONTINENTAL EVOLUTION AND GROWTH OF THE CENTRAL ASIAN FOLD BELT. Геодинамика и тектонофизика. 2017;8(3):421-427. https://doi.org/10.5800/GT-2017-8-3-0252

For citation:


Buslov M.M., Cai K. TECTONICS AND GEODYNAMICS OF THE ALTAI-JUNGGAR OROGEN IN THE VENDIAN-PALEOZOIC: IMPLICATIONS FOR THE CONTINENTAL EVOLUTION AND GROWTH OF THE CENTRAL ASIAN FOLD BELT. Geodynamics & Tectonophysics. 2017;8(3):421-427. https://doi.org/10.5800/GT-2017-8-3-0252

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