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Volume 30 Issue 5
Oct 2019
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Journal of Earth Science  > 2019  >  30(5): 1031-1040.
Pingping Zhu, Qiuming Cheng, Guoxiong Chen. New Fractal Evidence of Pacific Plate Subduction in the Late Mesozoic, Great Xing'an Range, Northeast China. Journal of Earth Science, 2019, 30(5): 1031-1040. doi: 10.1007/s12583-019-1216-y
Citation: Pingping Zhu, Qiuming Cheng, Guoxiong Chen. New Fractal Evidence of Pacific Plate Subduction in the Late Mesozoic, Great Xing'an Range, Northeast China. Journal of Earth Science, 2019, 30(5): 1031-1040. doi: 10.1007/s12583-019-1216-y
shu

New Fractal Evidence of Pacific Plate Subduction in the Late Mesozoic, Great Xing'an Range, Northeast China

doi: 10.1007/s12583-019-1216-y
  • 1.

    School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

  • 2.

    State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China

  • 3.

    State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

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  • Corresponding author: Qiuming Cheng
  • Received Date: 24 May 2018
  • Accepted Date: 20 Oct 2018
  • Publish Date: 01 Oct 2019
    Abstract
  • Late Mesozoic granitoids are widespread in the Great Xing'an Range (GXR), which is part of a large igneous province in eastern China. The geodynamic setting of the Late Mesozoic granitoids is still debated, and there have been two dominant models proposed, subduction and thermal erosion. This study discusses the geodynamic mechanisms from a new perspective on ages of the granitoids and fractal dimensions of their shape. Our results show that granitoids become gradually older from South GXR to North GXR to Erguna Block (EB) in the Jurassic, and opposite in the Cretaceous. The fractal dimensions of the Perimeter-area model (DAP) exhibit the same features. The values of DAP are smaller from South GXR (0.673 1) to North GXR (0.628 0) to EB (0.607 9) in the Jurassic, and larger from South GXR (0.609 6) to North GXR (0.630 2) to EB (0.639 9) in the Cretaceous. This implies that the geometrical irregularities of the granitoids are shaped by subduction rather than thermal erosion. These spatial variations could be best explained by the subduction of the Pacific Plate and consequent granitoid magmatism in the Late Mesozoic, thus providing a new fractal evidence for Pacific Plate subduction mechanism and opening a new possibility method for studing plate movement.

     

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