Journal of Tropical Oceanography ›› 2010, Vol. 29 ›› Issue (4): 63-70.doi: 10.11978/j.issn.1009-5470.2010.04.063cstr: 32234.14.j.issn.1009-5470.2010.04.063

• Marine geophysics • Previous Articles     Next Articles

Analysis of crustal average velocity and Moho depth beneath the onshore-offshore transitional zone in the northern South China Sea

XIA Shao-hong, QIU Xue-lin, ZHAO Ming-hui, XU Hui-long, SHI Xiao-bin   

  1. Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, CAS, Guangzhou 510301, China
  • Received:2009-05-08 Revised:2009-08-13 Online:2010-07-31 Published:2010-07-29
  • About author:夏少红(1981—), 男, 湖北省监利县人, 博士, 现为中国科学院南海海洋研究所助理研究员, 主要从事海洋地球物理与层析 成像结构研究。
  • Supported by:

    中国科学院海洋地质与环境重点实验室基金(MGE2009KG09); 国家自然科学基金(U0933006); 科技部“973”项目(2007CB
    411701); 中国科学院边缘海地质重点实验室基金(MSGL0704)

Abstract:

In order to study the crustal structure beneath the onshore-offshore transitional zone in the northern South China Sea, we carried out an onshore-offshore seismic experiment offshore of Hong Kong in 2004. Based on the data recorded by the permanent seismic stations in Guangdong Province and Hong Kong and by portable seismic stations on the Dangan Islands, we obtained a series of laterally homogeneous 2-D models using Pg and PmP phases for every station, determined the crustal average velocity, and constrained variations of Moho depth. The results show that the crustal average velocity is generally about 6.2km·s−1, which is lower than the global crustal average velocity of 6.45km·s−1. It suggests that a low velocity layer in the middle crust has developed the beneath onshore-offshore transitional zone in the northern South China Sea. However, the average crustal velocity of 6.7km·s−1 in the eastern part of the study area was higher than the global average velocity (6.45km·s−1) according to the data at the SHW station, which could imply magma underplating and a high velocity layer in the lower crust. The Moho depth was about 26−35km and gradually thinned from northwest to southeast. These results indicate the onshore-offshore transitional zone is the transitional boundary between the northern South China Sea and South China. By modeling and analyzing these data, we have obtained some new knowledge: a low velocity layer of middle crust was generally detected and no high velocity body of lower crust was found on land, while the opposite occurred at sea, namely high velocity body of lower crust was detected and no low velocity layer of middle crust was found; and the thickness of crust thinned from land to sea. These results have improved our understanding on crustal structure and tectonics of South China and the northern South China Sea.

Key words: onshore-offshore transitional zone, northern South China Sea, crustal average velocity, onshore-offshore seismic experiment, Moho