Volume 47 Issue 5
May  2022
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Li Zhiqiang, Yang Bo, Han Zijun, Huang Zhen, Wu Qingxun, 2022. Tectonic-Thermal Evolution of Meso-Cenozoic Rift Basin in South Yellow Sea, Offshore Eastern China: Implications for Basin-Forming Mechanism and Thermal Evolution of Source Rocks. Earth Science, 47(5): 1652-1668. doi: 10.3799/dqkx.2021.152
Citation: Li Zhiqiang, Yang Bo, Han Zijun, Huang Zhen, Wu Qingxun, 2022. Tectonic-Thermal Evolution of Meso-Cenozoic Rift Basin in South Yellow Sea, Offshore Eastern China: Implications for Basin-Forming Mechanism and Thermal Evolution of Source Rocks. Earth Science, 47(5): 1652-1668. doi: 10.3799/dqkx.2021.152
shu

Tectonic-Thermal Evolution of Meso-Cenozoic Rift Basin in South Yellow Sea, Offshore Eastern China: Implications for Basin-Forming Mechanism and Thermal Evolution of Source Rocks

doi: 10.3799/dqkx.2021.152

  • Tianjin Branch of China National Offshore Oil Corporation, Tianjin 300459, China

  • Received Date: 2021-09-22
  • Publish Date: 2022-05-25
    Abstract
  • The tectonic-thermal evolution history of the Meso-Cenozoic rift basin in the South Yellow Sea is established by using Advanced McKenzie geodynamic model and Easy%RoDL chemical kinetic model, combined with the deep crust and lithospheric mantle structure of the basin, the process of Meso-Cenozoic plate convergence and dispersion around the basin is analyzed. In addition, the genesis of low geothermal state, basin-forming mechanism and thermal evolution of source rocks in the basin are discussed. The results show that the crustal extension coefficient is of about 1.22 and the lithospheric mantle extension coefficient is of about 1.06. From the rift period to the present, the maximum heat flow value only decreased from 76 mW/m2 to 66 mW/m2, and the maximum geothermal gradient only decreased from 37 ℃/km to 30 ℃/km. It is revealed that the low geothermal state runs through the whole rift basin development stage for the first time. Low lithospheric mantle extension coefficient, deep non-mirror Moho distribution, the development stage of the basin are only in the far field tensile stress environment behind the arc, all indicate that the low intensity of lithospheric mantle extension and asthenosphere upwelling is low that is the fundamental reason for the continuous low geothermal state of the basin, and the deep thermal stress is not the main power source of the basin formation. According to the high crustal extension coefficient and the evolution of the detachment fault, it is suggested that the Indosinian and Yanshanian thrust fault regenerated to form the intra-crustal detachment system, and controlled the development of rift basin by simple shear deformation, which is the basic basin-forming mechanism. The main oil expulsion of the source rocks in the southern and northern depressions is the sedimentary period of the second member of the Sanduo Formation, and the thermal evolution of the source rocks ended since the Oligocene tectonic inversion. Paleo-buried depth and paleo-geothermal field jointly control the thermal maturity differences of source rocks at the present same depth in the southern and northern depressions.

     

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