Volume 47 Issue 9
Sep.  2022
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Article Navigation >  Earth Science  > 2022  >  47(9): 3389-3400
Wang Jianwei, Bao Jun, Cao Jianjun, Zhao Leqiang, Zeng Zhiping, Gong Yajun, Li Shouji, Li Songtao, 2022. Two Types of Strike‐Slip Fault Zones and Their Tectonic Deformation Patterns in the Central Junggar Basin. Earth Science, 47(9): 3389-3400. doi: 10.3799/dqkx.2022.032
Citation: Wang Jianwei, Bao Jun, Cao Jianjun, Zhao Leqiang, Zeng Zhiping, Gong Yajun, Li Shouji, Li Songtao, 2022. Two Types of Strike‐Slip Fault Zones and Their Tectonic Deformation Patterns in the Central Junggar Basin. Earth Science, 47(9): 3389-3400. doi: 10.3799/dqkx.2022.032
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Two Types of Strike‐Slip Fault Zones and Their Tectonic Deformation Patterns in the Central Junggar Basin

doi: 10.3799/dqkx.2022.032

  • Research Institute of Petroleum Exploration and Development, Shengli Oilfield Ranch Co., SINOPEC, Dongying 257000, China

  • Received Date: 2022-01-20
  • Publish Date: 2022-09-25
    Abstract
  • The strike-slip fault zone plays an important role in controlling the formation and distribution of large and medium oil and gas fields in the compressional superimposed basins in western China, which is also one of the difficult problems in the study. Based on the high-density 3D seismic data, a fine strike-slip fault zone interpretation and deformation pattern analysis of the Jurassic in the central Junggar basin using a variety of structural analysis techniques are conducted in this study. During the second episode of Yanshan tectonic movement, two types of strike-slip fault zones of NWW left-lateral compression-torsion and NE left-lateral tension-torsion were developed in the Jurassic. They were both composed of four groups of shear faults, which followed the simple left-lateral shear mode, but they were very different in their geometric characteristics and structural attributes. There is no conjugate shear relationship between NWW and NE strike-slip fault zones, but arc-shaped joint and merge in the blunt angle zone (about 135°). In the tectonic deformation, the arc-shaped joint action of two types of left-lateral strike-slip faults controlled torsion deformation and shear fracture in the deformation area, forming a large scale clockwise torsional structural system. The deformation pattern of torsional structure can be used as a reference for the study of intracontinental orogenic belts, and also provides a new idea for oil and gas exploration in compression-torsional basins.

     

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