Lithologic Reservoirs ›› 2026, Vol. 38 ›› Issue (4): 126-136.doi: 10.12108/yxyqc.20260411

• PETROLEUM EXPLORATION • Previous Articles     Next Articles

Reconstruction and petroleum exploration potential of the Permian prototype basin in the periphery of Fukang fault zone, Junggar Basin

WANG Yanjun1,2(), BIAN Baoli3, XIANG Hui4, ZHANG Yongjun5, SUN Yongxing6(), XU Xuelong4, MA Delong1,2, LI Yun7   

  1. 1 Research Institute of Petroleum Exploration & Development-Northwest(NWGI), PetroChina, Lanzhou 730020, China
    2 Key Laboratory of Reservoir Discription, CNPC, Lanzhou 730020, China
    3 Research Institute of Exploration and Development, PetroChina Xinjiang Oilfield Company, Karamay 834000, Xinjiang, China
    4 Zhundong Oil Production Plant, PetroChina Xinjiang Oilfield Company, Urumqi 830091, China
    5 Tuha Branch of Logging Co., Ltd., CNPC, Hami 839099, Xinjiang, China
    6 College of Tourism and Geographical Science, Leshan Normal University, Leshan 614000, Sichuan, China
    7 China University of Petroleum-Beijing at Karamay, Karamay 834000, Xinjiang, China
  • Received:2025-12-10 Revised:2026-03-24 Online:2026-07-01 Published:2026-07-06
  • Contact: SUN Yongxing E-mail:wang_yj8@petrochina.com.cn;yohance@126.com

Abstract:

To define the distribution range and resource exploration potential of Permian Lucaogou Formation source rocks in Fukang fault zone and its surrounding areas, based on the latest data of seismic, drilling, and high-precision gravity, the geological structure and tectonic evolution of Bogda piedmont were clarified. The basin configuration of Early-Middle Permian was reconstructed, and the resource scale of source rocks was assessed. Research results show that: (1) During Early-Middle Permian, Bogda and its adjacent areas underwent the evolution from a rift basin to a post-rift depression lacustrine basin, forming an paleo tectonic pattern of “alternating uplifts and sags”,which can be divided into four secondary tectonic units: Xiaoquangou uplift, Funan Sag, Jinan uplift and Jinan Sag, with the subsidence center of the lacustrine basin located south of the present-day Bogda Mountain. (2) From late Middle Permian to Himalayan period, multiple orogenic movements caused the structural inversion and dismemberment of the original lacustrine basin center,with continuous uplift of Bogda Mountain, resulting in a total horizontal shortening of about 62.2 km. (3) During the sedimentary period of Permian Lucaogou Formation, a deep lacustrine post rift depression lake basin was developed around Fukang fault zone. The total area of the prototype basin is about 153 7 km2, the resource scale of Lucaogou Formation in Jinan Sag is about 2.4 times that of Jimsar Sag, making it 10×108 ton oil shale exploration area. The reservoir formation model is “bilateral hydrocarbon supply, multi-layered stratified accumulation”. Jimsar Sag and Jinan Sag, serving as dual hydrocarbon source centers, have developed a vertically multi-stacked and laterally interconnected stratified accumulation system around Carboniferous volcanic paleo-uplifts weathered crusts, Middle Permian Lucaogou Formation shale oil, and Upper Permian Wutonggou Formation lithologic-stratigraphic traps.

Key words: prototype basin reconstruction, rift basin, depression lake basin, tectonic evolution, Lucaogou Formation, Permian, Jimsar Sag, Jinan Sag, Fukang fault zone, Junggar Basin

CLC Number: 

  • TE121.3

Fig. 1

Tectonic unit division of Fukang fault zone and its adjacent areas (a) and comprehensive stratigraphic column of Upper Paleozoic-Mesozoic in the southern margin (b), Junggar Basin"

Fig. 2

Seismic interpretation (a) and geological structure profile (b) across south-north direction of Fukang fault zone-Shaqi uplift"

Fig. 3

Seismic interpretation (a) and geological structure profile (b) across west-east direction of Fukang fault zone-Shaqi uplift"

Fig. 4

Remaining gravity anomaly map (a) and interpretation map of structural units (b) in the lower erosion layer of Jimsar Sag-Fukang fault zone"

Fig. 5

Seismic-geological section across Fukang fault zone-Jimsar Sag-Shaqi uplift"

Fig. 6

Recovery sequences of tectonic evolution profiles across Fukang fault zone-Jimsar Sag-Shaqi uplift"

Fig. 7

Evolution of Permian prototype basin across south-north direction of Fukang fault zone-Jimsar Sag-Shaqi uplift"

Fig. 8

Lithofacies paleogeography during the sedimentary period of Middle Permian Lucaogou Formation in eastern Junggar Basin"

Fig. 9

Hydrocarbon accumulation models of Bogda piedmont"

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