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Tectonic boundaries in the South China Sea from aeromagnetic signature

  • Geomorphology and geological structure of South China Sea
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Abstract

Magnetic data has been widely applied in the tectonic division. High-resolution magnetic data were used to analyze the geotectonic zoning of the South China Sea. Based on the newly compilated magnetic data, the processing results and the distribution of known faults, we consider that the U-shaped line approximately along the South China Sea national boundary of China shown in the magnetic map is a significant geological and geophysical boundary. We first described the linear characteristics of the magnetic data and then applied pseudo-gravity, Euler deconvolution, tilt derivatives, and the texture segmentation method to process the data. Results show that the dividing line between the South China Sea and the surrounding blocks is approximately along this U-shaped line. The dividing line between the South China domain and the South China Sea domain is along with the Dongsha Islands to Xisha Trough, which is different from the previous geophysical zoning results. Our results are almost consistent with those of the gravity data indicating roughly the tectonic zonation along the U-shaped line.

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Data Availability Statement

All data generated and/or analyzed during this study are available from the corresponding author upon reasonable request.

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Correspondence to Yao Luo.

Additional information

Supported by the Geological Survey Project of China (Nos. DD20191001, DD20191004, DD20189410) and the National Key R&D Program of China (No. 2017YFC0602000)

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Luo, Y., Yin, H., Liu, Q. et al. Tectonic boundaries in the South China Sea from aeromagnetic signature. J. Ocean. Limnol. 41, 550–561 (2023). https://doi.org/10.1007/s00343-022-2043-z

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  • DOI: https://doi.org/10.1007/s00343-022-2043-z

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