Journal of Tropical Oceanography ›› 2023, Vol. 42 ›› Issue (1): 135-144.doi: 10.11978/2022029CSTR: 32234.14.2022029

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Thickness and velocity structures of the carbonate platform sediments in the Xisha Islands constrained by receiver function method

HUANG Haibo1,2(), QIU Xuelin1,2,3, LONG Genyuan4,5, JIAO Dongfeng4,5, HAN Xiaohui4,5   

  1. 1. Key Laboratory of Ocean and Marginal Sea Geology (South China Sea Institute of Oceanology, Chinese Academy of Sciences), Guangzhou 511458, China
    2. Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China
    3. University of Chinese Academy of Sciences, Beijing 100049, China
    4. Hainan Key Laboratory of Marine Geological Resources and Environment, Haikou 570206, China
    5. Marine Geological Institute of Hainan Province, Haikou 570206, China
  • Received:2022-02-16 Revised:2022-04-10 Online:2023-01-10 Published:2022-04-15
  • Contact: HUANG Haibo. email: go223@scsio.ac.cn
  • Supported by:
    National Natural Science Foundation of China(42176081); Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)(GML2019ZD0204); Open Project of Hainan Key Laboratory of Marine Geological Resources and Environment(HNHYDZZYHJKF003); National Natural Science Foundation of China(41274110)

Abstract:

Thickness and elastic wave velocity are important parameters for evaluating the size and structural stability of coral reef. This study collected the receiver functions from two portable seismic stations on the Chenhang Island and Yongxing Island in the Xisha area, South China Sea. Travel times of the P-to-S converted waves and their multiple phases generated at the base of the carbonate platform are accurately picked up. At the same time, the thickness, average P-wave velocity, and velocity ratio of the carbonate platform sediments were calculated based on the drilling data and artificial seismic exploration results. The results show that the average P-wave velocity of the platform sediments on the Yongxing Island and Chenhang Island is about 3.5 km·s-1, the Vp/Vs ratio is 2.42, and the average thicknesses are about 1.35 km and 1.55 km, respectively. The calculated thicknesses are consistent with that of the well on the Yongxing Island which reaches the reef bottom at about 1.257 km. The sediment thickness of the Chenhang Island is slightly larger than that of the Yongxing Island (about 200m), which reflects the fluctuation of the basement beneath the island or is related to the reef growth faces.

Keywords carbonate platform; velocity structure; Vp/Vs ratio; receiver function; Xisha Islands