东喜马拉雅构造结东、西边界断裂对比及其构造演化过程

董汉文; 许志琴; 曹汇; 李源; 刘钊; 李化启; 易治宇; 陈希节; 马绪宣; 吴婵

doi:10.3799/dqkx.2018.701

Volume 43 Issue 4

Apr. 2018

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Article Navigation > Earth Science > 2018 > 43(4): 933-951

Dong Hanwen, Xu Zhiqin, Cao Hui, Li Yuan, Liu Zhao, Li Huaqi, Yi Zhiyu, Chen Xijie, Ma Xuxuan, Wu Chan, 2018. Comparison of Eastern and Western Boundary Faults of Eastern Himalayan Syntaxis, and Its Tectonic Evolution. Earth Science, 43(4): 933-951. doi: 10.3799/dqkx.2018.701

Citation:

Dong Hanwen, Xu Zhiqin, Cao Hui, Li Yuan, Liu Zhao, Li Huaqi, Yi Zhiyu, Chen Xijie, Ma Xuxuan, Wu Chan, 2018. Comparison of Eastern and Western Boundary Faults of Eastern Himalayan Syntaxis, and Its Tectonic Evolution. Earth Science, 43(4): 933-951. doi: 10.3799/dqkx.2018.701

Citation:

Dong Hanwen, Xu Zhiqin, Cao Hui, Li Yuan, Liu Zhao, Li Huaqi, Yi Zhiyu, Chen Xijie, Ma Xuxuan, Wu Chan, 2018. Comparison of Eastern and Western Boundary Faults of Eastern Himalayan Syntaxis, and Its Tectonic Evolution. Earth Science, 43(4): 933-951. doi: 10.3799/dqkx.2018.701

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Comparison of Eastern and Western Boundary Faults of Eastern Himalayan Syntaxis, and Its Tectonic Evolution

doi: 10.3799/dqkx.2018.701

1.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China
3.
Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2017-12-20
Publish Date: 2018-04-15

Abstract

Abstract

It is important to clarify the relationship between the eastern and western boundary faults of the eastern Himalayan syntaxis (EHS), and tectonic evolution of the eastern Himalayan syntaxis (EHS) since the collision of the Indian and Eurasian plates. Combined with field mapping, structure observations, zircon U-Pb geochronological investigations and previous studies of the EHS, this study identifies and describes the architecture and kinematics of the two boundary faults, discusses their multi-stage of deformation, also the evolution of the study area since the collision of Indian and Eurasian plates. The results show that the two boundary shear zones are similar in architecture and kinematics, and their tectonic deformation is obviously contemporaneous and in same stage, having experienced a series of important geological events, including the collision, subduction-exhumation and collapse-uplift.
- eastern Himalayan syntaxis,
- boundary fault,
- zircon LA-ICP-MS U-Pb dating,
- tectonics

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References(78)

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