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Characteristics and evolution of faults in the north-central Yin’e Basin and the effects on the coal-seam in the Cretaceous strata

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Abstract

Research on the characteristics of faults and their evolutionary history since the Cretaceous in the Suhongtu-Dagu depressions can provide a theoretical basis for geological evaluation of the coal seams in the Suhongtu Formation in the northern-central region of the Yin’e Basin. Using 3-D seismic-logging inversion techniques, seismic stratigraphic calibration, stratigraphic sequence delineation, and thickness calculations on the Suhongtu-Dagu depressions were carried out to clarify the planar and profile distributions of the faults, as well as the evolutionary history of these faults and the tectonic history of the depressions. The results of this study revealed that the distribution of the faults in the Suhongtu-Dagu depressions in the northern part of the Yin’e Basin varies with region, and the fault system was multi-period, orthotopic, north-east-trending, and north-north-east-trending, with a certain degree of inheritance in terms of the geological setting. Three types of faults were identified: Y-shaped fractures, reverse Y-shaped fractures, and parallel fractures, which can be classified as Paleozoic Cenozoic continuous syncline faults and intra-depression faults from the top of the Permian to the Upper Cretaceous series and inter-stratigraphic adjustment faults within the Cretaceous System, respectively. The evolution of these faults can be divided into three phases: the controlling faults were the faults that existed before the Early Cretaceous and had been active since then; synclinal faults that formed during the Early Cretaceous; and modified faults that formed since the Early Cretaceous. The development and modification of the coal seams in the Cretaceous Suhongtu Formation in the Hari, Kuanzihu, and Babei sags were strongly controlled and influenced by a multi-phase complex fault system.

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Acknowledgments

We thank LetPub for its linguistic assistance during the preparation of this manuscript. This work is granted by the National Natural Science Foundation of China (Grant No. 42272152), the Major Projects from the Changqing Oilfield of PetroChina (No. ZDZX2021), the Fundamental Research Funds for the Central Universities, CHD (No. 300102272205), the Fundamental Research Funds for platform of Liangshan Characteristic Agriculture (015/500827), and the Innovation and Entrepreneurship Training Program for University Students, CHD (No. G202210710050).

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Authors and Affiliations

  1. School of Earth Science and Resources, Chang’an University, Xi’an, 710054, China

    Qiang Yu, Xianyao Sun, Xianghe Lei, Ahmed Khaled & Qike Yang

  2. School of Information Technology, Xichang University, Xichang, 615013, China

    Baojiang Wang

  3. Department of geology, Northwest University, Xi’an, 710069, China

    Zhanli Ren

Authors
  1. Qiang Yu
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  2. Baojiang Wang
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  3. Zhanli Ren
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  6. Ahmed Khaled
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  7. Qike Yang
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Correspondence to Baojiang Wang or Zhanli Ren.

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Author Biographies

Qiang Yu, male, born in 1983 in Shaanxi Province, is currently an associate professor at the School of Earth Science and Resources, Chang’an University. His research interests focus on tectonothermal history recovery using thermochronology and geothermometry for petroleum accumulation and structural ore-forming model.

Baojiang Wang, born in 1970 in Ningxia Province, is currently an associate professor at the School of Information Technology, Xichang University. His research interests focus on structural geology using seismic data and reservoir prediction for petroleum exploration.

Zhanli Ren, born in 1961 in Shaanxi Province, is currently a professor at the Department of Geology, Northwest University. His research interests focus on tectonothermal history recovery and petroleum accumulation.

XianYao Sun, Xianghe Lei, Ahmed Khaled, and Qike Yang are all graduate students at the Chang’an University majoring in geology.

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Yu, Q., Wang, B., Ren, Z. et al. Characteristics and evolution of faults in the north-central Yin’e Basin and the effects on the coal-seam in the Cretaceous strata. Front. Earth Sci. 17, 30–44 (2023). https://doi.org/10.1007/s11707-022-1031-0

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