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Volume 35 Issue 3
Jun 2024
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Zheren Zhao, Shichao Li, Lingyu Zhang. Depositional Responses to the Mongol-Okhotsk Ocean Closure in the Central Area of the Great Xing'an Range: Insights into Thrust Faults and Foreland Basins. Journal of Earth Science, 2024, 35(3): 797-811. doi: 10.1007/s12583-023-1934-x
Citation: Zheren Zhao, Shichao Li, Lingyu Zhang. Depositional Responses to the Mongol-Okhotsk Ocean Closure in the Central Area of the Great Xing'an Range: Insights into Thrust Faults and Foreland Basins. Journal of Earth Science, 2024, 35(3): 797-811. doi: 10.1007/s12583-023-1934-x

Depositional Responses to the Mongol-Okhotsk Ocean Closure in the Central Area of the Great Xing'an Range: Insights into Thrust Faults and Foreland Basins

doi: 10.1007/s12583-023-1934-x
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  • Corresponding author: Shichao Li, lsc@jlu.edu.cn
  • Received Date: 22 Apr 2023
  • Accepted Date: 11 Sep 2023
  • Issue Publish Date: 30 Jun 2024
  • The Mongol-Okhotsk Ocean, which has been closing gradually from the west to the east beginning since the Late Paleozoic, was an important part of the Central Asian Orogenic Belt. It influenced the tectonic framework of Northeast Asia in the Mesozoic, especially the Late Mesozoic arc-basin system that is widely distributed in the Great Xing'an Range. However, the manner in which the Mongol-Okhotsk Ocean affected the sedimentary basin development remains poorly understood. To address this issue, we conducted U-Pb dating of detrital zircon deposited sedimentary basins of the central Great Xing'an Range. By examining the possible provenances of the detrital zircon and the structural controls of the basins, we found that a key sedimentary unit was deposited around Late Jurassic–Early Cretaceous. Its provenance was a felsic source in a back-arc setting of an active continental margin. The findings also suggest the existence of a unified geodynamic setting that affected the coeval development of basins in the northern Great Xing'an Range and the Yanshan fold-thrust belt along the northern margin of North China Craton. This research helps to better understand the complex tectonic processes which shaped the Northeast Asia during the Late Mesozoic.

     

  • Electronic Supplementary Materials: Supplementary materials (ESM Ⅰ Tables S1–S2, ESM Ⅱ Figures S1–S6) are available in the online version of this article at https://doi.org/10.1007/s12583-023-1934-x.
    Conflict of Interest
    The authors declare that they have no conflict of interest.
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