Lithologic Reservoirs ›› 2024, Vol. 36 ›› Issue (1): 121-135.doi: 10.12108/yxyqc.20240112

• PETROLEUM EXPLORATION • Previous Articles     Next Articles

Lithofacies paleogeography evolution of Late Ordovician in Sichuan Basin and its surrounding areas

SUN Hanxiao1, XING Fengcun1,2, XIE Wuren3, QIAN Hongshan4   

  1. 1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China;
    2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China;
    3. PetroChina Research Institute of Petroleum Exploration and Development, Beijing 100083, China;
    4. Research Institute of Exploration and Development, PetroChina Southwest Oil and Gas Field Company, Chengdu 610041, China
  • Received:2023-02-04 Revised:2023-02-26 Online:2024-01-01 Published:2024-01-02

Abstract: Based on outcrops, cores, drilling and logging data, the evolution process of Lithofacies paleogeography of Late Ordovician in Sichuan Basin and its surrounding areas was described and compared, and the main controlling factors were discussed. The results show that:(1) The early Caledonian tension-extension led to the deepening of the depression around the study area, and then the collision and extrusion of the Yangtze plate and Cathaysia block formed the paleogeographic pattern of the upper Late Ordovician Yangtze region as the center, surrounded by uplifts on the northwest, west and south sides.(2) The Late Ordovician in Sichuan Basin and its surrounding areas can be divided into(mixed) shore, carbonate gentle slope and(mixed) shelf sedimentary facies. The Baota Formation-Linxiang Formation mainly developed carbonate gentle slope facies. At the transgressive peak of Wufeng Formation, the carbonate gentle slope was submerged and developed(mixed) shelf deep water black shale. The regressions of Guanyinqiao Formation led to the transition from deep shelf to shallow shelf subfacies in most areas. There are(mixed) shore facies developed in the periphery of paleo-uplift in all periods, and some areas affected by provenance have mixed sedimentary characteristics.(3) The lithofacies paleogeographic pattern of the Late Ordovician in the study area is controlled by multiple factors such as tectonic movement, sea level change and paleoclimate, which is reflected in the plane distribution and vertical evolution of sedimentary facies.

Key words: (mixed)shore, carbonate gentle slope, (mixed)shelf, lithofacies paleogeography, sedimentary evolution, Baota Formation-Linxiang Formation, Wufeng Formation, Guanyinqiao Formation, Late Ordovician, Sichuan Basin

CLC Number: 

  • TE122.2
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