Earth Science Frontiers ›› 2023, Vol. 30 ›› Issue (5): 420-429.DOI: 10.13745/j.esf.sf.2023.2.75

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Recover the Liyue Basin position in the southern margin of the South China Sea before seafloor spreading

CHEN Wenlin1(), ZHENG Qiugen1,*(), HUANG Yiming2, ZHANG Yi1, LIN Changsong1   

  1. 1. School of Ocean Sciences, China University of Geosciences (Beijing), Beijing 100083, China
    2. Shale Oil and Gas Department, Shenyang Geological Survey Center, China Geological Survey, Shenyang 110034, China
  • Received:2023-03-01 Revised:2023-03-23 Online:2023-09-25 Published:2023-10-20
  • Contact: ZHENG Qiugen

Abstract:

Based on the conceptions that magnetic stripping is symmetrical about a mid-ocean ridge axis and that magnetic stripes from the same period are isochronic, using the existing magnetic anomaly data of the South China Sea, and assuming the positions of the South China Block and the northern margin of the South China Sea are relatively fixed and the southern margin of the South China Sea began to drift southward since 32 Ma, this paper restores the seafloor spreading history of the South China Sea and recovers the relative position of the Liyue Basin in various periods. The Liyue Basin was located next to the southeast rim of the Pearl River Mouth Basin before seafloor spreading. This finding is further supported by the comparison results of basement properties, development and sedimentary characteristics of Mesozoic strata, as well as Cenozoic tectonic activities and subsidence and sedimentary characteristics between the Liyue Basin and the northern margin basin of the South China Sea. This study provides an essential reference for the structural evolution, sedimentary filling characteristics, sediment source analysis, and petroleum geological conditions of the Liyue Basin.

Key words: southern margin of the South China Sea, northern margin of the South China Sea, Liyue Basin, position recovery, Pearl River Mouth Basin, Qiongdongnan Basin

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