Deep Duplex Thrust in the Sangzhi-Shimen Tectonic Belt, in the West Hunan and Hubei Areas

Xuliang Zhang; Dengfa He

doi:10.1007/s12583-019-0873-1

Volume 31 Issue 1

Jan 2020

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Journal of Earth Science > 2020 > 31(1): 79-90.

Xuliang Zhang, Dengfa He. Deep Duplex Thrust in the Sangzhi-Shimen Tectonic Belt, in the West Hunan and Hubei Areas. Journal of Earth Science, 2020, 31(1): 79-90. doi: 10.1007/s12583-019-0873-1

Citation:

Xuliang Zhang, Dengfa He. Deep Duplex Thrust in the Sangzhi-Shimen Tectonic Belt, in the West Hunan and Hubei Areas. Journal of Earth Science, 2020, 31(1): 79-90. doi: 10.1007/s12583-019-0873-1

Xuliang Zhang, Dengfa He. Deep Duplex Thrust in the Sangzhi-Shimen Tectonic Belt, in the West Hunan and Hubei Areas. Journal of Earth Science, 2020, 31(1): 79-90. doi: 10.1007/s12583-019-0873-1

Citation:

Xuliang Zhang, Dengfa He. Deep Duplex Thrust in the Sangzhi-Shimen Tectonic Belt, in the West Hunan and Hubei Areas. Journal of Earth Science, 2020, 31(1): 79-90. doi: 10.1007/s12583-019-0873-1

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Deep Duplex Thrust in the Sangzhi-Shimen Tectonic Belt, in the West Hunan and Hubei Areas

doi: 10.1007/s12583-019-0873-1

Xuliang Zhang^{,
,},
Dengfa He

School of Energy Resources, China University of Geosciences, Beijing 100083, China

More Information

Corresponding author: Xuliang Zhang
Received Date: 09 Jan 2019
Accepted Date: 11 May 2019
Publish Date: 01 Feb 2020

Abstract

Abstract

Recent studies indicate that there is a large buried body developing in the Sangzhi-Shimen tectonic belt, which is between the Xuefeng intracontinental deformation system and the Xiangexi tectonic belt. In order to explore the tectonic evolution and main deformation-controlling factors of the buried body, we carried out a series of studies and built two new models based on the latest seismic data and fault-related fold theory. These new models show that the deformation of the buried body in the north segment of the study area is different from that in the middle-south segment. After further study, we found the main factors leading to these differences were:(1) the magnitude of the principal stress, (2) the range of tectonic movements, and (3) the morphology and depth of the basement detachment. Subsequently, with the physical simulation experiments, a 3D evolution model of the study area was built.
- Sangzhi-Shimen tectonic belt,
- concealed structures,
- deformation-controlling factors,
- basement detachment,
- evolution model,
- faulting

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References(32)

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Deep Duplex Thrust in the Sangzhi-Shimen Tectonic Belt, in the West Hunan and Hubei Areas

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Deep Duplex Thrust in the Sangzhi-Shimen Tectonic Belt, in the West Hunan and Hubei Areas

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