Xinjiang Petroleum Geology ›› 2008, Vol. 29 ›› Issue (6): 722-724.

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Tectonic-Lithofacies Zone and Hydrocarbon Accumulation in Wuerhe-Xiazijie Area of Northwestern Margin of Junggar Basin

JIANG Chun-ling1, XU Duo-nian1, WANG Wei-feng2, HAN Neng-run3   

  1. 1. Northwest Branch, Research Institute of Exploration and Development, PetroChina, Lanzhou, Gansu 730020, China;
    2. China University of Petroleum, Dongying, Shandong 257061, China;
    3. Well Logging Company, Western Drilling Engineering Corporation, CNPC, Karamay, Xinjiang 834000, China
  • Received:2008-03-07 Published:2020-11-20

Abstract: Wuerhe-Xiazijie area is divided into nine structural units, and has nine sedimentary facies types and three sedimentary systems. The different structural zones allowed to developing different sedimentary systems. The growth fault caused the differences in sedimentary thickness of isochron strata and in sedimentary system in two sides of the fault. The fault's strike controlled the distribution directions of the sedimentary systems, and the step thrust faults formed multiple steep fan-delta. Wuerhe anticline fan-delta front (middle alluvial fan), Wuerhe-Xiazijie-Karameli thrust belt fan-delta plain (root alluvial fan), Xiazijie-Hongqiba bruchfalten zone fan-delta plain (root alluvial fan) tectonic-lithofacies zones are favorable locations for hydrocarbon accumulation.

Key words: Junggar basin, Wuerhe, Xiazijie, structural system, tectonic-lithofacies zone, hydrocarbon accumulation

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