西藏的缝合带与特提斯演化

曾庆高; 王保弟; 西洛郎杰; 毛国正; 刘海永; 刘恭喜

doi:10.3799/dqkx.2020.152

Volume 45 Issue 8

Aug. 2020

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Article Navigation > Earth Science > 2020 > 45(8): 2735-2763

Zeng Qinggao, Wang Baodi, Xiluo Langjie, Mao Guozheng, Liu Haiyong, Liu Gongxi, 2020. Suture Zones in Tibetan and Tethys Evolution. Earth Science, 45(8): 2735-2763. doi: 10.3799/dqkx.2020.152

Citation:

Zeng Qinggao, Wang Baodi, Xiluo Langjie, Mao Guozheng, Liu Haiyong, Liu Gongxi, 2020. Suture Zones in Tibetan and Tethys Evolution. Earth Science, 45(8): 2735-2763. doi: 10.3799/dqkx.2020.152

Zeng Qinggao, Wang Baodi, Xiluo Langjie, Mao Guozheng, Liu Haiyong, Liu Gongxi, 2020. Suture Zones in Tibetan and Tethys Evolution. Earth Science, 45(8): 2735-2763. doi: 10.3799/dqkx.2020.152

Citation:

Zeng Qinggao, Wang Baodi, Xiluo Langjie, Mao Guozheng, Liu Haiyong, Liu Gongxi, 2020. Suture Zones in Tibetan and Tethys Evolution. Earth Science, 45(8): 2735-2763. doi: 10.3799/dqkx.2020.152

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Suture Zones in Tibetan and Tethys Evolution

doi: 10.3799/dqkx.2020.152

1.
Tibet Bureau of Geological and Mineral Exploration and Development, Lhasa 850000, China
2.
Chengdu Center of China Geological Survey, Chengdu 610081, China
3.
West Exploration Group, Tibet Bureau of Geological and Mineral Exploration and Development, Lhasa 851400, China
4.
Tibet Geological Survey, Lhasa 850000, China
5.
Geothermal Geological Brigade, Tibet Bureau of Geological and Mineral Exploration and Development, Lhasa 851400, China

Received Date: 2020-04-26
Publish Date: 2020-08-15

Abstract

Abstract

The study of suture zones in Tibet is always one of the hottest scientific problems related to the fundamental geology of Tibetan Plateau. Based on the composition, tectonic and formation ages for the four suture zones in the Tibetan Plateau, and through the analysis of spatial-temporal structure, it is proposed that the evolution of the Paleo-Tethys was related to the transform faults. The expansion of the Yarlung Zangbo Ocean Basin shows space-time transformation coupled with the Indosinian orogeny in the Qiangtang-Sanjiang area. Focusing on the Paleo-Tethys and Neo-Tethys transformation and expansion properties of the Bangong-Nujiang belt, it is found in this study that its tectonic mechanism is left-lateral strike-slip and pull-apart, which have resulted in a series of extensional complexes parallel to the strike-slip and pull-apart, and so it is as important as that of the thrust back sliding detachment system on the basin-ridge metamorphic core complex in the western United States. In this paper, it also discusses the difference of geological structures in eastern and western Tibet, and proposes that the expansion and widening of the Gangdese magmatic arc were constrained by the double subduction of the Yarlung Zangbo Tethys Ocean.
- suture zone,
- transform fault,
- strike-slip boundary,
- Proto-Tethys,
- Paleo-Tethys,
- Neo-Tethys,
- structural geology

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References(290)

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