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    Volume 48 Issue 10
    Oct.  2023
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    Tong Qinlong, Ye Fawang, Qin Mingkuan, 2023. U-Pb Chronology of Detrital Zircons from Lower Cretaceous in Xinniwusu Sag, Bayingobi Basin and Its Geological Significance. Earth Science, 48(10): 3613-3630. doi: 10.3799/dqkx.2021.198
    Citation: Tong Qinlong, Ye Fawang, Qin Mingkuan, 2023. U-Pb Chronology of Detrital Zircons from Lower Cretaceous in Xinniwusu Sag, Bayingobi Basin and Its Geological Significance. Earth Science, 48(10): 3613-3630. doi: 10.3799/dqkx.2021.198

    U-Pb Chronology of Detrital Zircons from Lower Cretaceous in Xinniwusu Sag, Bayingobi Basin and Its Geological Significance

    doi: 10.3799/dqkx.2021.198
    • Received Date: 2021-08-29
      Available Online: 2023-10-31
    • Publish Date: 2023-10-25
    • Petrography, whole rock geochemistry, and in-situ U-Pb dating of the detrital zircons from the sandstones of the uranium-bearing target formation in the Xinniwusu sag of the Bayingobi basin were used to limit the sedimentary age and provenance of Lower Cretaceous of Bayingobi Formation, and constrain the relationship between the Early Cretaceous basins and mountains and the source of uranium minerals. Photomicrographs show that the formation has the characteristics of proximal deposition. The characteristics of K, Rb, La, Th, Zr, Sc, Hf, REE and their ratios indicate that the source rocks are mainly intermediate-acid rocks from different tectonic backgrounds. The peak ages of detrital zircons are mainly 430 Ma, 250 Ma and 270 Ma, and the youngest is 125±1 Ma. Combined with the K-Ar age of the basalt in the overlying Cretaceous Suhongtu Formation, the sedimentation age of the upper member of Bayingobi Formation in the study area was limited to (125±1)-(111.3±2.1) Ma. The lower part of the upper member of the Bayingobi Formation in the northern part of the Xinniwusu sag are mainly derived from Shandamiao and Wubulage areas in the northeastern Langshan. In the middle part, the provenance mainly comes from Wuliji, Shangdan and Tukmu uplift of the Shalazhashan structural belt. The provenance of the upper member of Bayingobi Formation in the southern part of the Xinniwusu sag mainly comes from the Nuru-Honggueryulin structural belt in the south and the Shalazhashan uplift in the north. The provenance area changed obviously in the middle part of the Upper Bayingobi Formation indicates that differential uplift and decline occurred in the Bayingobi basin during the late Early Cretaceous. The northeastern part to the study area was relatively declined, while the southwestern part was relatively uplifted, which changed the principal direction of sediment source from the northeast in the early to the west and east.

       

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