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    中国百强科技报刊

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    Volume 49 Issue 1
    Jan.  2024
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    Article Navigation >  Earth Science  > 2024  >  49(1): 123-139
    Tian Gang, Yang Minghui, Song Lijun, Xing Zhou, Bai Donglai, Chen Jie, Li Jingying, 2024. New Understanding of Basement Structural Characteristics and Its Evolution Process in Ordos Basin. Earth Science, 49(1): 123-139. doi: 10.3799/dqkx.2022.193
    Citation: Tian Gang, Yang Minghui, Song Lijun, Xing Zhou, Bai Donglai, Chen Jie, Li Jingying, 2024. New Understanding of Basement Structural Characteristics and Its Evolution Process in Ordos Basin. Earth Science, 49(1): 123-139. doi: 10.3799/dqkx.2022.193
    shu

    New Understanding of Basement Structural Characteristics and Its Evolution Process in Ordos Basin

    doi: 10.3799/dqkx.2022.193
    • 1.

      Shaanxi Coalfield Geophysical Prospecting and Surveying Co. Ltd., Xi'an 710005, China

    • 2.

      College of Geosciences, China University of Petroleum, Beijing 102249, China

    • 3.

      State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249, China

    • 4.

      School of Earth Sciences and Engineering, Xi'an Shiyou University, Xi'an 710065, China

    • 5.

      Command Center of Natural Resource Comprehensive Survey, China Geological Survey, Beijing 100055, China

    • Received Date: 2022-03-05
      Available Online: 2024-01-24
    • Publish Date: 2024-01-25
      Abstract
    • In order to understand the characteristics of basement structure in Ordos Basin, using 1∶200 000 magnetic data and seismic data, combined with the latest research progress of rock assemblage, rock magnetism, chronology and rock geochemistry of basement rock samples and Precambrian metamorphic rock series around the basin, the characteristics of basement primary faults and basement structure are studied in detail. On the basis of defining the age attributes of each basement area in the basin, the Paleoproterozoic tectonic evolution process of the basement is restored. The basement structure of the basin is controlled by four primary faults, which are divided into five secondary structural units. The lithology of each structural unit is the extension of the peripheral Archean-Paleoproterozoic to the basin. The high magnetic anomaly zones are mostly reflected by the Archean blocks, and the negative aeromagnetic anomaly zones are mostly reflected by the Paleoproterozoic sedimentary metamorphic rocks, showing the characteristics of NE horizontal blocking. The Paleoproterozoic tectonic evolution process includes the early stage of northern ocean crust subduction (> 2.2 Ga); subduction-back arc and NE extension-supracrustal rock deposition stage (~2.2-1.95 Ga); Yinshan Block and Ordos Block collision-NE closing of arc basin-forming western block stage (~1.95-1.85 Ga); eastern block collided with the eastern part of the western block-NE trending tectonic reformation-formation the Trans North China Orogen (~1.85-1.80 Ga).

       

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