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    Volume 48 Issue 1
    Jan.  2023
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    Article Navigation >  Earth Science  > 2023  >  48(1): 293-316
    Li Xiangbo, Liu Huaqing, Yang Weiwei, Zhang Yan, Carlos Zavala, Ji Limin, Yang Zhanlong, Hao Bin, Huang Junping, Wang Jing, 2023. A Lacustrine Basin Driven by Extreme Events of Alternate Dry-Wet Climatic Cycles: Evidence from Outcrops of Yanchang Formation in Upper Triassic, Ordos Basin. Earth Science, 48(1): 293-316. doi: 10.3799/dqkx.2022.463
    Citation: Li Xiangbo, Liu Huaqing, Yang Weiwei, Zhang Yan, Carlos Zavala, Ji Limin, Yang Zhanlong, Hao Bin, Huang Junping, Wang Jing, 2023. A Lacustrine Basin Driven by Extreme Events of Alternate Dry-Wet Climatic Cycles: Evidence from Outcrops of Yanchang Formation in Upper Triassic, Ordos Basin. Earth Science, 48(1): 293-316. doi: 10.3799/dqkx.2022.463
    shu

    A Lacustrine Basin Driven by Extreme Events of Alternate Dry-Wet Climatic Cycles: Evidence from Outcrops of Yanchang Formation in Upper Triassic, Ordos Basin

    doi: 10.3799/dqkx.2022.463
    • 1.

      PetroChina Research Institute of Petroleum Exploration & Development-Northwest, Lanzhou 730020, China

    • 2.

      Key Laboratory of Petroleum Reservoir Description, PetroChina, Lanzhou 730020, China

    • 3.

      Exploration and Development Institute of PetroChina Changqing Oilfield Company, Xi'an 710018, China

    • 4.

      GCS Argentina, Molina Campos 150, Bahía Blanca 8000, Argentina

    • 5.

      Departamento de Geología, Universidad Nacional del Sur, San Juan 670, Bahía Blanca 8000, Argentina

    • 6.

      Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China

    • Received Date: 2022-09-08
      Available Online: 2023-02-01
    • Publish Date: 2023-01-25
      Abstract
    • The Ordos Basin is one of the main petroliferous basins in China. The Triassic Yanchang Formation is the main oil-bearing units in this basin. Based on the investigation and study of typical outcrops of Yanchang Formation and the data of paleontology, lithology and lithofacies, three new insights are obtained. (1) The paleoclimatic environment of Yanchang Formation during the sedimentary period has been recovered, which is considered to be tripartite, and the Ladinian Age was an arid environment. During the Carnian Age, the climate changed to a warm and humid environment because of the Carnian Pluvial Episode (CPE). In the Norian-Rhaetian ages, the climate environment changed to semi-arid and sub-humid again. (2) The CPE changed the way of sediment transport and deposition in the Yanchang Formation. In the dry environment period before and after the CPE, the seasonal river, crevasse splay and crevasse channels caused by rainstorm and flood were mainly developed. During the CPE and in the mid-Carnian period, terrigenous detrital materials were transported to the underwater environment mainly by various gravity flows such as turbidity flow, sandy debris flow and hyperpycnal flow, forming sandy event deposits. At the same time, controlled by the CPE, black organic-rich shale event deposits were also developed in the deep water environment. (3) Two sedimentary models of arid and humid environments were established in the Yanchang Formation. In the former, the catchment area in the arid environment was small, and the main sedimentary units were flood plain, seasonal channel, crevasse splay, crevasse channels and so on. In the latter, the catchment area of the humid environment is large, and the complete continental fluvial, delta-lacustrine and gravity flow sedimentary system is developed. Due to the stable long-flowing water, the channel is relatively fixed, the sedimentation mode is mainly progradation, supplemented by retrogradation, and not obvious aggradation. The study is of practical value to the discussion of how the large depressed lake basin formed and evolved in the Yanchang Formation, sedimentary sequence evolution, and petroleum exploration, and it is also significant to the study of the sedimentological records in inland lake basins generated by global extreme climate events in the Late Triassic Epoch to understand the sedimentary responses of the Carnian Pluvial Episode in the Pangea at the east margin of the Paleo-Tethys.

       

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