Lithologic Reservoirs ›› 2024, Vol. 36 ›› Issue (5): 56-66.doi: 10.12108/yxyqc.20240506

• PETROLEUM EXPLORATION • Previous Articles     Next Articles

Provenance transformation and sedimentary filling response of Mesozoic in Halahatang-Hade area，Tarim Basin

YI Zhenli1,2,3, SHI Fang1,2,3, YIN Taiju4, LI Bin1,2,3, LI Meng1,2,3, LIU Liu1,2,3, WANG Zhukun1,2,3, YU Ye5   

  1. 1. Research Institute of Exploration and Development, PetroChina Tarim Oilfield Company, Korla 841000, Xinjiang, China;
    2. R & D Center for Ultra-Deep Complex Reservoir Exploration and Development, CNPC, Korla 841000, Xinjiang, China;
    3. Engineering Research Center for Ultra-deep Complex Reservoir Exploration and Development, Xinjiang Uygur Autonomous Region, Korla 841000, Xinjiang, China;
    4. School of Geosciences, Yangtze University, Wuhan 430100, China;
    5. School of Earth Sciences and Spatial Information Engineering, Hunan University of Science and Technology, Xiangtan 411201, Hunan, China
  • Received:2023-07-13 Revised:2023-08-10 Online:2024-09-01 Published:2024-09-04

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Abstract: The sediment supply and infilling evolution of the Mesozoic in Halahatang-Hade area of Tarim Basin were studied by analyzing the changes in paleogeomorphic morphology，distribution of sedimentary systems， stratigraphic structure and sand-bodies development characteristics，based on the main measuring method of mineral composition analysis，calculation of sand to land ratio，seismic attribute analysis and logging response feature recognition. The results show that：（1）The provenance of the Triassic mainly came from the Tianshan orogenic belt in the northeast，with ZTR coefficient gradually increasing from the northern area to the central sag. During the Jurassic and Cretaceous，the provenance mainly came from the orogenic belt of Kunlun Mountains in the southeast and south. The ZTR coefficient of this period is gradually increasing from the northern and southern areas to the central sag.（2）In the late Triassic，with the proliferation of the Paleo-Tethys Ocean，the weakening of the uplift of the Tianshan Mountains in the north of the study area and the intensification of the uplift of the Kunlun Mountains in the south are the main reasons for this provenance transformation.（3）During the Triassic，the depression and deposition centers were located in the south of the study area，and a set of braided river delta and deep-water lake deposits in the NE-SW direction were mainly developed. During the Jurassic and Cretaceous，the depression and deposition centers migrated to the north of the study area，and a set of braided river delta and shallow lake deposits were developed in the direction of SE-NW and S-N respectively.（4）During the Triassic，the progradation direction of sand-bodies was mainly in the NE-SW direction. During the Jurassic and Cretaceous，the progradation direction of sand-bodies was mainly in the SE-NW and S-N direction respectively.（5）The exploration areas for Triassic lithologic reservoirs are located in the southwest of the study area，while the exploration areas for Jurassic and Cretaceous lithologic reservoirs are located in the northwest and north of the study area.

Key words: provenance transformation, sedimentary filling-stacking pattern, seismic attribute, ZTR coefficient of heavy mineral, intensity of uplift, lithologic reservoirs, Mesozoic, Halahatang-Hade area, Tarim Basin

CLC Number: 

  • TE121.3+2
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