Lithologic Reservoirs ›› 2024, Vol. 36 ›› Issue (6): 89-97.doi: 10.12108/yxyqc.20240609

• PETROLEUM EXPLORATION • Previous Articles     Next Articles

Stratigraphic division of astronomical cycle in early-middle Jurassic Shuixigou Group in the Shengbei subsag of Tuha Basin

GOU Honguang1, LIN Tong2, FANG Qiang3,4, ZHANG Hua1, LI Shan3,4, CHENG Yi1, You Fan1   

  1. 1. Research Institute of Exploration and Development, Tuha Oilfield Company, PetroChina, Hami 839009, Xinjiang, China;
    2. Research Institute of Petroleum Exploration and Development, PetroChina, Beijing, 100083, China;
    3. State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences(Beijing), Beijing 100083, China;
    4. School of Ocean Sciences, China University of Geosciences(Beijing), Beijing 100083, China
  • Received:2024-03-20 Revised:2024-05-21 Online:2024-11-01 Published:2024-11-04

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Abstract: The natural gamma-ray（GR）logging data of the early-middle Jurassic Shuixigou Group from QinTan 1 borehole in Shengbei subsag，Tuha basin，was selected to analyze cyclostratigraphy and simulate sedimentary noise for the identification of stratigraphic Milankovitch signals and determination of the Earth’s orbital cycle’s forcing the lake level variations within the Tuha Basin. The stratigraphic division of Shuixigou Group was ana lyzed. The results show that：（1）The sedimentary cycles of 12.8～51.1 m，3～11.9 m，1.1～3.6 m，and 1.3～ 2.4 m were identified in the GR curves of the Early-Middle Jurassic Shuixigou Group in the Shengbei subsag of Tuha Basin，with a ratio of 21∶5∶1.5∶1，and the sedimentary rates of the Shuixigou Group are estimated as 3.6～ 11.7 cm·ka-1 through astronomical calibration and correlation coefficient.（2）The sedimentary records of the Shuixigou Group were forced by the Milankovitch cycles，as evidenced by the presence of 405 ka long eccentricity， 99～131 ka short eccentricity，32.6～35.0 ka obliquity，and 20.0～24.8 ka precession cycles during the Middle and Early Jurassic in Tuha basin. The durations of Badaowan Formation（not drilled through），Sangonghe Formation and Xishanyao Formation in Qintan 1 borehole are 3.0 ±0.1 Ma，4.1 ±0.1 Ma and 9.0 ±0.1 Ma， respectively.（3）The fluctuation of lake level forced by the Earth’s orbital cycles of terrestrial lake basins，the simulation of lake level change by sedimentary noise confirms that the ultra-long period of ～1.5 Ma forced the lake level change of the Shuixigou Group in Taibei sag.

Key words: cyclostratigraphy, Milankovitch cycles, astronomical time scale, sedimentary rate, simulate sedimentary noise, lake level variations, Shuixigou Group, Jurassic, Shengbei subsag, Tuha Basin

CLC Number: 

  • TE121.3
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