CSCD来源期刊

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中国科技核心期刊

地学领域高质量科技期刊分级T2区（2023）

世界期刊影响力指数报告Q1区（2023）

Volume 42 Issue 1
Jan.  2023
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Article Navigation >  Bulletin of Geological Science and Technology  > 2023  >  42(1): 226-238
Cao Zicheng, Tang Daqing, Luo Mansong, Jiang Zhongzheng, Hong Caijun, Xia Yongtao, Wei Hua. Structural characteristics and tectonic evolution of Mesozoic-Cenozoic faults in the Shunbei area, Tarim Basin[J]. Bulletin of Geological Science and Technology, 2023, 42(1): 226-238. doi: 10.19509/j.cnki.dzkq.2022.0176
Citation: Cao Zicheng, Tang Daqing, Luo Mansong, Jiang Zhongzheng, Hong Caijun, Xia Yongtao, Wei Hua. Structural characteristics and tectonic evolution of Mesozoic-Cenozoic faults in the Shunbei area, Tarim Basin[J]. Bulletin of Geological Science and Technology, 2023, 42(1): 226-238. doi: 10.19509/j.cnki.dzkq.2022.0176
shu

Structural characteristics and tectonic evolution of Mesozoic-Cenozoic faults in the Shunbei area, Tarim Basin

doi: 10.19509/j.cnki.dzkq.2022.0176
  • 1.

    Exploration and Development Research Institute, Northwest Oilfield Branch, SINOPEC, Urumqi 830011, China

  • 2a.

    School of Earth Resources, China University of Geosciences(Wuhan), Wuhan 430074, China

  • 2b.

    Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences(Wuhan), Wuhan 430074, China

  • 3.

    Research Institute of Petroleum Exploration & Development, Tarim Oil Field, Korla Xinjiang 841000, China

  • Received Date: 13 Jul 2021
    Abstract

  • Oil and gas resources in the Shunbei area of the Tarim Basin are rich in Paleozoic strata.Recent petroleum exploration indicates that Mesozoic-Cenozoic sedimentary rocks have a good potential in hydrocarbon extraction. In this study, recently acquired 3D seismic surveys were used to systematically analyze fault types, geometrical characteristics, and evolution of Mesozoic-Cenozoic faults in the Shunbei area. The objective is to understand the characteristics and development mechanisms of faults that have the key controlling factors of hydrocarbon accumulation.In the Shunbei area, the dominant faults are tensional normal faults with few thrust faults and strike-slip faults. The district has many small scale, disorderly distributed faults. Combined with the regional setting and basin evolution stage, we suggest that the development of Mesozoic-Cenozoic faults in the Shunbei area experienced three tectonic cycles during the Indosinian, Yanshanian, and Himalayan periods. The structural position, middle Permian igneous rocks, and the sandy mudstone of the Lower Triassic Tongketuer Formation have significant control on fault evolution.Detailed interpretation of faults in the T90-T50 stratigraphic interval in the Shunbei area shows that the central part of the No.5 fault and south central part of the No.7 fault are two large faults that connect downward to the source rock of the basin. In these two areas, some faults cut upward through T90 to T50, which is good forvertical migration of hydrocarbon from Paleozoic to Mesozoic-Cenozoic strata and therefore are ideal locations for petroleum exploration.

     

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