新疆石油地质 ›› 2020, Vol. 41 ›› Issue (zk(English)): 92-100.

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Deformation Mechanism of Hutubi Anticline in the Southern Margin of Junggar Basin: Insights From Physical Simulation Experiment

ZHANG Xichen1, MA Delong1, WEI Lingyun2, WANG Hongbin1, WANG Yanjun1, LIU Wenqiang1, YANG Xiulei1   

  1. 1. PetroChina, a. Key Laboratory of Reservoir Description; b. Northwest Branch, Research Institute of Petroleum Exploration and Development, Lanzhou, Gansu 730020, China;
    2. Geophysics Institute, Research Institute of Exploration and Development, Xinjiang Oilfield Company, PetroChina, Urumqi, Xinjiang 830013, China
  • 出版日期:2021-01-01 发布日期:2021-09-14

Deformation Mechanism of Hutubi Anticline in the Southern Margin of Junggar Basin: Insights From Physical Simulation Experiment

ZHANG Xichen1, MA Delong1, WEI Lingyun2, WANG Hongbin1, WANG Yanjun1, LIU Wenqiang1, YANG Xiulei1   

  1. 1. PetroChina, a. Key Laboratory of Reservoir Description; b. Northwest Branch, Research Institute of Petroleum Exploration and Development, Lanzhou, Gansu 730020, China;
    2. Geophysics Institute, Research Institute of Exploration and Development, Xinjiang Oilfield Company, PetroChina, Urumqi, Xinjiang 830013, China
  • Online:2021-01-01 Published:2021-09-14
  • About author:ZHANG Xichen, E-mail:zhangxchen@petrochina.com.cn

摘要: The fold-thrust belts in the southern margin of Junggar basin are characterized by multi-stage superimposition and deformation. The Hutubi anticline located in the front of the thrust is far away from the Tianshan Mountains and shows a double-layer structure, among which the deep layer is a Permian fault-depression-paleohigh and the shallow layer is a fault anticline of Jurassic with its overlying strata. To investigate the main controls on the shallow anticline formation and the vertical deformation mechanism of the Hutubi anticline, 5 groups of models are designed to perform physical simulation study by using control variable and comparative analysis methods on the basis of the identification of structural style and deformation laws. The study results show that the experimental result of the fault-depression-paleohigh model is similar to the seismic interpretation result. As the main controlling factor, the paleohigh in the fault-depression margin induced the overlying strata to deform into anticlines, which can prove the time-space coupling relations between the deep layer and shallow layer in the Hutubi anticline. The shape of the shallow anticline is also controlled by the combination of the scale of the underlying fault-depression, the overlying strata thickness and the syntectonic sedimentation. It is a scientific and effective method to reveal the correlation and deformation mechanism of vertical superimposed structures by using physical simulation experiments, which could provide more basis for petroleum exploration and production in the foreland area of the southern margin of Junggar basin.

关键词: Junggar basin, Hutubi anticline, deformation mechanism, physical simulation, pre-existing fault-depression, paleohigh, overlying strata thickness, syntectonic sedimentation, controlling factor

Abstract: The fold-thrust belts in the southern margin of Junggar basin are characterized by multi-stage superimposition and deformation. The Hutubi anticline located in the front of the thrust is far away from the Tianshan Mountains and shows a double-layer structure, among which the deep layer is a Permian fault-depression-paleohigh and the shallow layer is a fault anticline of Jurassic with its overlying strata. To investigate the main controls on the shallow anticline formation and the vertical deformation mechanism of the Hutubi anticline, 5 groups of models are designed to perform physical simulation study by using control variable and comparative analysis methods on the basis of the identification of structural style and deformation laws. The study results show that the experimental result of the fault-depression-paleohigh model is similar to the seismic interpretation result. As the main controlling factor, the paleohigh in the fault-depression margin induced the overlying strata to deform into anticlines, which can prove the time-space coupling relations between the deep layer and shallow layer in the Hutubi anticline. The shape of the shallow anticline is also controlled by the combination of the scale of the underlying fault-depression, the overlying strata thickness and the syntectonic sedimentation. It is a scientific and effective method to reveal the correlation and deformation mechanism of vertical superimposed structures by using physical simulation experiments, which could provide more basis for petroleum exploration and production in the foreland area of the southern margin of Junggar basin.

Key words: Junggar basin, Hutubi anticline, deformation mechanism, physical simulation, pre-existing fault-depression, paleohigh, overlying strata thickness, syntectonic sedimentation, controlling factor