克拉通内走滑断裂空间结构及派生构造新样式：以塔里木盆地顺北12号断裂为例

何松高; 邓尚; 刘雨晴; 邱华标; 朱秀香; 李传新

doi:10.3799/dqkx.2022.495

Volume 48 Issue 6

Jun. 2023

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He Songgao, Deng Shang, Liu Yuqing, Qiu Huabiao, Zhu Xiuxiang, Li Chuanxin, 2023. New Structural Style of Spatial Architecture and Derived Structure of Intracratonic Strike-Slip Faults: A Case Study of Shunbei No. 12 Fault, Tarim Basin. Earth Science, 48(6): 2136-2150. doi: 10.3799/dqkx.2022.495

Citation:

He Songgao, Deng Shang, Liu Yuqing, Qiu Huabiao, Zhu Xiuxiang, Li Chuanxin, 2023. New Structural Style of Spatial Architecture and Derived Structure of Intracratonic Strike-Slip Faults: A Case Study of Shunbei No. 12 Fault, Tarim Basin. Earth Science, 48(6): 2136-2150. doi: 10.3799/dqkx.2022.495

Citation:

He Songgao, Deng Shang, Liu Yuqing, Qiu Huabiao, Zhu Xiuxiang, Li Chuanxin, 2023. New Structural Style of Spatial Architecture and Derived Structure of Intracratonic Strike-Slip Faults: A Case Study of Shunbei No. 12 Fault, Tarim Basin. Earth Science, 48(6): 2136-2150. doi: 10.3799/dqkx.2022.495

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New Structural Style of Spatial Architecture and Derived Structure of Intracratonic Strike-Slip Faults: A Case Study of Shunbei No. 12 Fault, Tarim Basin

doi: 10.3799/dqkx.2022.495

He Songgao^{1, 2
,
,},
Deng Shang^{2, 3
,
,},
Liu Yuqing²,
Qiu Huabiao²,
Zhu Xiuxiang³,
Li Chuanxin¹

1.
School of Energy Resources, China University of Geosciences, Beijing 100083, China
2.
SINOPEC Petroleum Exploration and Production Research Institute, Beijing 100083, China
3.
SINOPEC Northwest Oilfield Company, Urumqi, 830011, China

Received Date: 2022-09-21
Publish Date: 2023-06-25

Abstract

Abstract

With the acquisition of high-precision continuous 3D seismic data, the intracratonic strike-slip faults with medium to small slip displacements reveal complex spatial structure and structural style. In this study it carries out detailed analysis on the three-dimensional spatial structure, kinematic characteristics and movement periods of the Shunbei No. 12 fault and its formation mechanism. The results show follows: (1) The compressional deformation of the first-order strike-slip faults in the Shunbei area gradually increases from the west to the east. Among these strike-slip faults, the Shunbei No. 12 fault is located in a transitional position in the NE-trending strike-slip fault system. In terms of structural style, both the "pull-up structure, strike-slip segment, and push-up structure" segmented structure and the "pressure ridge structure" of the faults to the west and to the east, respectively, are developed. (2) In the north of the carbonate rock top surface of Shunbei No. 12 fault, NE 20° trending branch faults are developed. The upper en echelon normal faults are strongly active, forming a fan-shaped geometry. The lower fault is characterized by steeply dipping faults, forming into a new structural style. (3) Under the influence of tectonic events at the plate boundaries, the Shunbei No. 12 fault and its derived branches experienced three stages of left lateral strike slip movements: in the third episode of the Middle Caledonian period, the Shunbei No. 12 fault and the branch faults were initiated. In the Late Caledonian period, multiple fault planes were activated and interacted with each other, dragging the overlying strata to form the first series of en echelon normal fault. In the Middle Hercynian period, the second series of en echelon normal faults were formed.
- pressure ridge structurel,
- layered deformation,
- activity period,
- structural style,
- strike-slip fault,
- Tarim basin,
- petroleum geology

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References(56)

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New Structural Style of Spatial Architecture and Derived Structure of Intracratonic Strike-Slip Faults: A Case Study of Shunbei No. 12 Fault, Tarim Basin

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