Lithologic Reservoirs ›› 2023, Vol. 35 ›› Issue (4): 145-160.doi: 10.12108/yxyqc.20230414

• PETROLEUM EXPLORATION • Previous Articles     Next Articles

Sedimentary characteristics of shallow water delta of Middle Jurassic Toutunhe Formation in southern Anjihai river outcrops，Junggar Basin

FU Wenjun1, ZHANG Changmin1, JI Dongsheng2, LOU Lin2, LIU Jiale1, WANG Xulong2   

  1. 1. School of Geoscience, Yangtze University, Wuhan 430100, China;
    2. PetroChina Xinjiang Oilfield Company, Karamay 830013, Xinjiang, China
  • Received:2022-08-10 Revised:2022-09-01 Online:2023-07-01 Published:2023-07-01

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Abstract: The Middle Jurassic Toutunhe Formation is an important exploration target zone in the southern margin of Junggar Basin. Based on the field survey of southern Anjihai river outcrops in the southern margin of Junggar Basin，combined with thin section identification of rock samples and geochemical analysis data，the lithologies and sedimentary structure of Toutunhe Formation were descried，and the sedimentary environment，sedimentary facies types and depositional evolution were analyzed. The results show that：（1）The Middle Jurassic Toutunhe Formation in the study area experienced a semi-arid，arid and humid climate evolution during the sedimentary period. The lacustrine basin was shallow，the lake bottom was gentle，and shallow delta deposits were developed.（2）Six types of sedimentary microfacies were developed in the study area，including distributary channel，inter-distributary depression，underwater distributary channel，inter-distributary bay，sheet sand and beach bar. The shallow water delta of Toutunhe Formation was affected by rivers and lake waves，forming a river-dominated shallow water delta in the stable period of lacustrine basin，and wave-dominated shallow water delta was developed.（3）From the early stage to the late stage of Toutunhe Formation，the lake level generally decreased and then increased. Riverdominated shallow water delta was developed in the first member of Toutunhe Formation，the distributary channel had strong hydrodynamic force. The river was frequently diverted and bifurcated，and continuously accumulated towards the lacustrine basin. The multi-stage channels were spliced. At that time，it was dominated by distributary channel and underwater distributary channel. Subsequently，the climate was further dry，wave-controlled shallow water delta was developed in the second member of Toutunhe Formation. The river action was weakened，and the wave action was enhanced. The delta plain was dominated by the development of a folded distributary channel. The sand bodies of underwater distributary channel of the delta front were transformed by wave scouring，forming strip-shaped sheet sand. During the deposition of the third member of Toutunhe Formation， due to the continuous subsidence of the Junggar Basin and the lateral migration of delta lobes，the surface of delta lobes in the shallow lacustrine basin was covered by lake water，and part of the clastic materials in the front of the shallow delta were reconstructed by lake waves， forming beach bar deposits parallel to the lake shore.

Key words: shallow water delta, river-dominated, wave-dominated, sedimentary facies, depositional model, Toutunhe Formation, Middle Jurassic, Junggar Basin

CLC Number: 

  • TE122.1
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