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    Volume 49 Issue 1
    Jan.  2024
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    Article Contents
    Gao Chonglong, Wang Jian, Liu Ming, Luo Zhengjiang, Wang Ke, Liu Ke, Ren Ying, Deng Yi, 2024. Boundary Changes of Jurassic-Cretaceous Prototype Basin of Southern Junggar and Responses of Sedimentary Provenance and Depositional Systems. Earth Science, 49(1): 103-122. doi: 10.3799/dqkx.2022.076
    Citation: Gao Chonglong, Wang Jian, Liu Ming, Luo Zhengjiang, Wang Ke, Liu Ke, Ren Ying, Deng Yi, 2024. Boundary Changes of Jurassic-Cretaceous Prototype Basin of Southern Junggar and Responses of Sedimentary Provenance and Depositional Systems. Earth Science, 49(1): 103-122. doi: 10.3799/dqkx.2022.076

    Boundary Changes of Jurassic-Cretaceous Prototype Basin of Southern Junggar and Responses of Sedimentary Provenance and Depositional Systems

    doi: 10.3799/dqkx.2022.076
    • Received Date: 2021-11-18
      Available Online: 2024-01-24
    • Publish Date: 2024-01-25
    • In order to clarify the characteristics and provenance-sedimentary system of the J-K prototype basin in southern Junggar, in this study it firstly analyzes the age data of mountains along the basin margin, and the temporal-spatial changes of Jurassic-Cretaceous sandstone clastic composition, conglomerate gravel composition, heavy minerals, paleo-currents, sedimentary sand body distribution. Then the original basin boundary distances are quantitively calculated. Together with the regional geological background, the boundary changes, and sedimentary provenance and depositional system evolution of the Jurassic-Cretaceous prototype basin in southern Junggar are restored. The research results show that the uplifting time of the mountains in the western section of the southern Junggar is overall earlier than the middle and eastern sections. And the parent rocks of the Jurassic-Cretaceous sedimentary provenance are mainly recirculating orogenic belt sedimentary rock. The distance between the boundary of prototype and nowadays basins is 22.2-67.0 km. The western section of southern Junggar is controlled by north and south provenance systems and influenced by the evolution of Chemo paleouplift. And the basin boundary has showed shrinking processes since Middle Jurassic. The middle section of southern Junggar is controlled by southern provenance system, and the basin boundary continuously expanded from the Early Jurassic to early period of the Middle Jurassic, and then began to shrink. In contrast, the basin boundary of eastern section continuously shrunk during the whole Jurassic. However, uplift processes of the Bogda Mountain since the Middle Jurassic have caused significant changes in the regional provenance-sedimentary system. Overall, current areas of the western and eastern sections are closer to the prototype basin boundary during the Late Jurassic, therefore, the proximal sedimentary systems are relatively well developed. However, the locations of the mid part of southern Junggar during the whole Jurassic are far from the original basin boundary, consequently, the contiguous sand bodies of proximal sedimentary are not well developed. In the Early Cretaceous, the boundaries of the southern Junggar basically shrunk to the vicinity of present basin boundary, but regional lacustrine flooding can lead to relatively regress of locations of the provenance area.

       

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