巴颜喀拉构造带二叠—三叠纪岩相特征及构造演化

陈守建; 李荣社; 计文化; 赵振明; 李国栋; 刘荣丽; 戴传固; 朱迎堂

doi:10.3799/dqkx.2011.044

Volume 36 Issue 3

May 2011

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Article Navigation > Earth Science > 2011 > 36(3): 393-408

CHEN Shou-jian, LI Rong-she, JI Wen-hua, ZHAO Zhen-ming, LI Guo-dong, LIU Rong-li, DAI Chuan-gu, ZHU Ying-tang, 2011. Lithostratigraphy Character and Tectonic-Evolvement of Permian-Trias in the Bayankala Tectonic Belt. Earth Science, 36(3): 393-408. doi: 10.3799/dqkx.2011.044

Citation:

CHEN Shou-jian, LI Rong-she, JI Wen-hua, ZHAO Zhen-ming, LI Guo-dong, LIU Rong-li, DAI Chuan-gu, ZHU Ying-tang, 2011. Lithostratigraphy Character and Tectonic-Evolvement of Permian-Trias in the Bayankala Tectonic Belt. Earth Science, 36(3): 393-408. doi: 10.3799/dqkx.2011.044

Citation:

CHEN Shou-jian, LI Rong-she, JI Wen-hua, ZHAO Zhen-ming, LI Guo-dong, LIU Rong-li, DAI Chuan-gu, ZHU Ying-tang, 2011. Lithostratigraphy Character and Tectonic-Evolvement of Permian-Trias in the Bayankala Tectonic Belt. Earth Science, 36(3): 393-408. doi: 10.3799/dqkx.2011.044

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Lithostratigraphy Character and Tectonic-Evolvement of Permian-Trias in the Bayankala Tectonic Belt

doi: 10.3799/dqkx.2011.044

1.
Xi'an Institute of Geology and Mineral Resources, Xi'an 710054, China
2.
Guizhou Institute of Geological Survey, Guiyang 550005, China
3.
Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China

Received Date: 2010-07-15
Publish Date: 2011-05-01

Abstract

Abstract

Tethys Ocean formation and evolvement poses one of the important foundamental geological issues in studies concerning the Tibetan Plateau Integrating the field work, data analysis, previous studies, and particularly with the 1∶250 000 regional geology data, in Bayankala tectonic belt during Permian-Trias, including the normal stratum, lithofacies character and tectonic-paleogeography, we discussed the tectonic evolvement in order to improve the research level of the Tethys ocean development in Tibetan Plateau and Rodinia continent formation. The Permian-Neogene's stratum appears in the main body of Bayankala tectonic belt, characterized by disappearing portion of Trias stratum before Permian. Permian-Trias stratum was continuously aggraded in ocean environment. Bayankala Group is distributed widely and formatting thick in Trias in continent and ocean environment being flysch and little volcanic sediment. Jurassic-Quaternary aggraded in continent formatting river and lake environment. Huangyangling Group aggraded in shallow and deep ocean environment formatting carbonate and fragmentary rock. It evolved from ocean environment to continent environment during Permian-Trias after collision, orogenesis and the blue water vanish, as the north part of main double ocean region contrasting with the south Longmu lake-Shuanghu ocean of Palaeo Tethys ocean lying between Talimu-China-Korea plate and south big continent (Gangwana continent).
- Bayankala tectonic belt,
- Permian-Trias,
- tectonic-paleogeography,
- Palaeo Tethys ocean,
- main ocean,
- tectonic evolution

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Lithostratigraphy Character and Tectonic-Evolvement of Permian-Trias in the Bayankala Tectonic Belt

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