Journal of Tropical Oceanography ›› 2022, Vol. 41 ›› Issue (1): 204-214.doi: 10.11978/2021028CSTR: 32234.14.2021028

• Marine Geophysics • Previous Articles    

Property analysis and lithology identification of seismic reflection anomalies on the continental slope of northeastern South China Sea

LI Bo’an1,2,3(), HU Shanzheng4, YAN Pin1,2, YU Junhui1,2, WANG Xiao5, TANG Qunshu1,2()   

  1. 1. Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences, Guangzhou 510301, China
    2. Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China
    3. University of Chinese Academy of Sciences, Beijing 100049, China
    4. Bureau of Geophysical Prospecting INC., China National Petroleum Corporation, Chengdu 610213, China
    5. Hainan Branch Company of CNOOC (China) Ltd, Haikou 570311, China
  • Received:2021-03-03 Revised:2021-04-07 Online:2022-01-10 Published:2021-04-13
  • Contact: TANG Qunshu E-mail:liboan18@mails.ucas.ac.cn;tqsh@scsio.ac.cn
  • Supported by:
    Youth Innovation Promotion Association Chinese Academy of Sciences(Y202076);Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)(GML2019ZD0204);Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)(GML2019ZD0104);Rising Star Foundation of the South China Sea Institute of Oceanology(NHXX2019DZ0101);Special Support Program for Cultivating High-level Talents in Guangdong Province(2019BT02H594);National Natural Science Foundation of China(U1901217);National Natural Science Foundation of China(91855101);National Natural Science Foundation of China(41876052)

Abstract:

The northern margin of the South China Sea (SCS) is often regarded as a magma-poor passive continental margin. Many high amplitude anomalies were observed in previous studies on seismic profiles at the northern part of the Continent-Ocean Transition (COT) in the northern SCS, and were interpreted as sills and volcanos. However, further investigation on the properties of these high amplitude anomalies was lacking. In this study, we observed a large anomaly with a thickness of ~1.2 km in two multi-channel seismic profiles (SO1E and SOY) on the northeastern continental slope of the SCS. This provides an opportunity to determine the presence of magmatic activities north of the COT. Velocity analysis and AVO (amplitude variation with offset) analysis were performed for the large-amplitude anomaly. Results show that the high-amplitude anomaly has a higher P wave velocity and Poisson’s ratio than the host strata above. Considering the regional geologic background, the internal reflection characteristics, spatial size and shape of this high-amplitude anomaly, we suggest that the high-amplitude anomaly can be characterized as an igneous rock and further classified as a laccolith. This also indicates that multi-phase magmatism occurred north of the COT since the Miocene.

Key words: northeastern South China Sea, laccolith, velocity analysis, AVO analysis

CLC Number: 

  • P738.4