塔里木盆地塔北地区深层走滑断裂分段性成因机制

冯建伟; 郭宏辉; 汪如军; 昌伦杰; 王超; 高翔

doi:10.3799/dqkx.2023.110

Volume 48 Issue 7

Jul. 2023

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Article Navigation > Earth Science > 2023 > 48(7): 2506-2519

Feng Jianwei, Guo Honghui, Wang Rujun, Chang Lunjie, Wang Chao, Gao Xiang, 2023. Segmentation Genesis Mechanism of Strike-Slip Fracture of Deep Carbonate Rocks in Tabei Area, Tarim Basin. Earth Science, 48(7): 2506-2519. doi: 10.3799/dqkx.2023.110

Citation:

Feng Jianwei, Guo Honghui, Wang Rujun, Chang Lunjie, Wang Chao, Gao Xiang, 2023. Segmentation Genesis Mechanism of Strike-Slip Fracture of Deep Carbonate Rocks in Tabei Area, Tarim Basin. Earth Science, 48(7): 2506-2519. doi: 10.3799/dqkx.2023.110

Citation:

Feng Jianwei, Guo Honghui, Wang Rujun, Chang Lunjie, Wang Chao, Gao Xiang, 2023. Segmentation Genesis Mechanism of Strike-Slip Fracture of Deep Carbonate Rocks in Tabei Area, Tarim Basin. Earth Science, 48(7): 2506-2519. doi: 10.3799/dqkx.2023.110

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Segmentation Genesis Mechanism of Strike-Slip Fracture of Deep Carbonate Rocks in Tabei Area, Tarim Basin

doi: 10.3799/dqkx.2023.110

1.
School of Geosciences, China University of Petroleum, Qingdao 266580, China
2.
Tarim Oilfield, PetroChina, Korla 841000, China

Received Date: 2021-11-29
Publish Date: 2023-07-25

Abstract

Abstract

The segmental characteristics of the deep strike-slip fault zone in the Tarim Basin are the key issues in the study of fault zone reservoir control, which is of great significance for promoting deep oil and gas exploration and development. From the perspective of the integration of the development characteristics of the Harahatang fault zone and the results of seismic data interpretation, in this study it discusses the segmentation characteristics of the Ha-15 fault zone in the Harahatang area of Tabei by carefully characterizing the structure and structural style of the Harahatang fault zone. On the basis of clarification of characteristics and stress state of the strike-slip motion of the fault zone in the north of the tower, the causal mechanism of the orderly development of secondary R' shear fracture and T-tensile fracture of deep strike-slip fracture is reasonably explained by taking the Coulomb-Anderson pure shear model and the Riddle single shear model as the framework, and combining the rock fracture criteria of Griffith and Coulomb-Moir. Finally, according to the structural analysis of the Harb-15 fault zone, a typical model of convergent strike-slip fault and derived tectonic development in the passive strike-slip tectonic environment is established. It is believed that the attenuation of regional extrusion stress and the change of three-way stress state are the main reasons for the segmentation of strike-slip fractures, which can be divided into compression torsion zone, torsion zone and tensile torsion zone along the direction of extrusion stress, and can be subdivided into linear tight closure fault combination zone, linear braided structural zone, symmetrical plume fault zone, stretch/extrusion laminate zone or oblique tensile division plot and horsetail fault combination zone.
- Tabei area,
- strike⁃slip segmentation,
- stress attenuation,
- rock fracture guideline,
- geomechanics

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References(71)

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Segmentation Genesis Mechanism of Strike-Slip Fracture of Deep Carbonate Rocks in Tabei Area, Tarim Basin

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