中国板块构造格局在早古生代末的重大转变

黄少英; 谢会文; 侯贵廷; 杨宪彰; 罗彩明; 张昊; 仲子奇; 夏金凯; 李祥; 常海宁

doi:10.3799/dqkx.2022.394

Volume 48 Issue 4

Apr. 2023

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Article Navigation > Earth Science > 2023 > 48(4): 1321-1329

Huang Shaoying, Xie Huiwen, Hou Guiting, Yang Xianzhang, Luo Caiming, Zhang Hao, Zhong Ziqi, Xia Jinkai, Li Xiang, Chang Haining, 2023. Key Transition of Chinese Plate Configuration at the End of Early Paleozoic. Earth Science, 48(4): 1321-1329. doi: 10.3799/dqkx.2022.394

Citation:

Huang Shaoying, Xie Huiwen, Hou Guiting, Yang Xianzhang, Luo Caiming, Zhang Hao, Zhong Ziqi, Xia Jinkai, Li Xiang, Chang Haining, 2023. Key Transition of Chinese Plate Configuration at the End of Early Paleozoic. Earth Science, 48(4): 1321-1329. doi: 10.3799/dqkx.2022.394

Citation:

Huang Shaoying, Xie Huiwen, Hou Guiting, Yang Xianzhang, Luo Caiming, Zhang Hao, Zhong Ziqi, Xia Jinkai, Li Xiang, Chang Haining, 2023. Key Transition of Chinese Plate Configuration at the End of Early Paleozoic. Earth Science, 48(4): 1321-1329. doi: 10.3799/dqkx.2022.394

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Key Transition of Chinese Plate Configuration at the End of Early Paleozoic

doi: 10.3799/dqkx.2022.394

1.
Institute of Petroleum Exploration and Development, Tarim Oilfield Company, Korla 841000, China
2.
Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China

Received Date: 2022-05-18
Publish Date: 2023-04-25

Abstract

Abstract

The plate configuration is the basic geological question in the tectonics, which considers the large scale basin-orogen relationship, and controls the configuration of oceans and continents, origin and evolution of basin-range provinces, and has also been applied to uncover the close of ocean and uplift of mountains. The end of Early Paleozoic is the key transition period of Chinese three plates. Based on the global high coefficient paleomagnetic data and tectonic comparison in geological affiliation, the global configuration in the Late Precambrian to Early Paleozoic is reconstructed by GPlate software, the Ordovician-Silurian is the key transition period of Chinese three plates. Before 440 Ma, the configuration of Chinese three plates is N-S/T style(North China lies in the west, South China lies in the northeast, Tarim lies in the southeast). After 440 Ma, the configuration is transformed into a T-N/S style (Tarim lies in the west, North China lies in the northeast, South China lies in the southeast) that maintains. The key transition is related to the breakup of the Late Precambrian Rodinian supercontinent and the change of ocean-continent configuration of Chinese three plates in the Early Paleozoic, the transition is from extension to compression in tectonic setting.
- Tarim,
- North China,
- South China,
- change of paleo-latitude,
- geological affinity,
- structural geology

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References(41)

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