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Geological Journal of China Universities ›› 2022, Vol. 28 ›› Issue (3): 424-439.DOI: 10.16108/j.issn1006-7493.2021010

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Study of 1-D Velocity Structure of Hydrate in Shenhu Area, South China Sea: Based on the Constraints of the Hydrate Zone with Moderate to Low Saturation

LIU Leifeng1, 5,XIA Shaohong1, 2*,FANG Yunxin2, 3,LIN Lin2, 3,FAN Chaoyan1, 2,SUN Jinlong4, Zhao Fang1, 2   

  1. 1. CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology,
    Chinese Academy of Sciences, Guangzhou 510301, China;
    2. Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China;
    3. Guangzhou Marine Geological Survey, China Geological Survey, Guangzhou 510075, China;
    4. Chinese Academy of Sciences Guangzhou Branch, Guangzhou 510070, China;
    5. University of Chinese Academy of Sciences, Beijing 100049, China
  • Online:2022-06-20 Published:2022-06-23

Abstract: As a common technical means of hydrate research, high-precision OBS surveys can obtain the fine-scale velocity structure of hydrate orebody, which is important for studying gas hydrate saturation, prediction and development of hydrate resources. However, forward simulation of OBS velocity structure is a tedious and time-consuming process, and constructing a reasonable initial model is an important prerequisite for subsequent fast fine-scale structure imaging. Based on data from18 hydrate areas in the world where velocity structures have been identified, this study analyzed the common characteristics and influencing factors of P-wave velocity in hydrate orebodies, and obtained the empirical formula of P-wave velocity in hydrate orebody zone with seawater depth and sediment thickness. Based on the empirical formula, OBS data and multi-channel seismic profiles, an initial model of Shenhu hydrate area is established, and a one-dimensional P-wave velocity structure of Shenhu sea area is obtained by ray tracing and travel-time fitting. The results show that Shenhu hydrate orebody has high P-wave velocity (1.83-1.92 km/s), and free gas has low P-wave velocity (1.60-1.70 km/s). In addition, the empirical formula can serve as an important reference for the simulation of the velocity structure in Shenhu area, and it is expected to provide a reliable initial model for obtaining the two-dimensional / three-dimensional velocity structures in Shenhu sea area so as to guide fine-scale explorations and resource assessments of hydrate.

Key words: gas hydrate, division of different zones, empirical formula, initial model, travel-time fitting, velocity structure