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    Volume 48 Issue 11
    Nov.  2023
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    Xiao Xuewei, Chen Honghan, Xu Ke, Su Ao, Yu Wenquan, 2023. Quantitative Cyclostratigraphy Analysis and Constraint by U-Pb Dating of Bedding-Parallel Fibrous Calcite Vein in Gaoyou Sag, Subei Basin. Earth Science, 48(11): 4088-4102. doi: 10.3799/dqkx.2022.122
    Citation: Xiao Xuewei, Chen Honghan, Xu Ke, Su Ao, Yu Wenquan, 2023. Quantitative Cyclostratigraphy Analysis and Constraint by U-Pb Dating of Bedding-Parallel Fibrous Calcite Vein in Gaoyou Sag, Subei Basin. Earth Science, 48(11): 4088-4102. doi: 10.3799/dqkx.2022.122

    Quantitative Cyclostratigraphy Analysis and Constraint by U-Pb Dating of Bedding-Parallel Fibrous Calcite Vein in Gaoyou Sag, Subei Basin

    doi: 10.3799/dqkx.2022.122
    • Received Date: 2021-05-24
      Available Online: 2023-11-30
    • Publish Date: 2023-11-25
    • Due to the lack of stable radioisotopic chronoscope in sedimentary strata for a long time, determination of their absolute ages has become the bottleneck both in stratigraphic and petroleum geological investigations. In this paper it uses quantitative cyclostratigraphy theory and method, combining with the constraint by U-Pb dating of bedding-parallel fibrous calcite, to re-determine the absolute age of the main statigraphic interfaces of the Gaoyou sag in Subei basin, and obtains the different duration of Sanduo movement and the coupling relationship in time between the structural transforming surface of dual rifting stages and the Pacific plate subduction bending (50 Ma±).The top and base of Sanduo Formation in Gaoyou sag are 34.0 Ma and 43.3 Ma respectively. The base of Dainan Formation is 50.5 Ma and that of Fu 1 and Fu 2 Members are 66.0 Ma and 56.5 Ma individually. The duration of residual strata of Sanduo Formation from Yong'an 38, which is in the sub-sag area, is 8.28 Ma, and its starting age of uplift denudation is 34.06 Ma, while the end is 23.03 Ma, which means the denudation time is 11.03 Ma. The time of denudation of uplift and slope was earlier than 34.06 Ma, and the time of denudation was longer. The U-Pb dating of Fu 4 member is 53.1±3.7 Ma. The results show follows: (1) The 50 Ma± and 23.03 Ma± interfaces in Gaoyou sag of the Subei basin are tectonic responses of the Pacific plate subduction bending and the collision between the Indian plate and the Eurasian plate. The depocenter of Gaoyou sag early uplifted comparatively since the Late Eocene (34.06 Ma) and underwent the denudation span of 11.03 Ma. The main reason is perhaps related to the remote effect of the overall performance of Indo-Eurasian plate collision with compression regime in the South China block, and lack of NE-trending deep mantle uplift. (2) The U-Pb dating result of bedding-parallel fibrous calcite veins developed in the source rock system can be used as the sedimentary age of the strata, providing an excellent anchor point constraint for quantitative cyclostratigraphic analysis of sedimentary basins.

       

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