Journal of Tropical Oceanography ›› 2010, Vol. 29 ›› Issue (4): 56-62.doi: 10.11978/j.issn.1009-5470.2010.04.056cstr: 32234.14.j.issn.1009-5470.2010.04.056

• Marine geophysics • Previous Articles     Next Articles

Associated interpretation of sub-bottom and single-channel seismic profiles from slope of Shenhu Area in the northern South China Sea—characteristics of gas hydrate sediment

LI Shou-jun1, 2, CHU Feng-you2, FANG Yin-xia2, WU Zi-yin2, NI Yu-gen3   

  1. 1.Graduate Department, China University of Geosciences, Wuhan 430074, China; 2. Second Institute of Oceanography, Key Lab of Submarine Geosciences, SOA, Hangzhou 310012, China; 3.Guangzhou Marine Geological Survey, Guangzhou 510760,China
  • Received:2009-07-27 Revised:2009-11-18 Online:2010-07-31 Published:2010-07-29
  • About author:李守军(1977—), 男, 黑龙江省方正县人, 助理研究员, 博士研究生, 主要从事海洋地球物理、天然气水合物调查研究工作。
  • Supported by:

    国家海洋局第二海洋研究所基本科研业务费专项(JG0705); 国家青年基金东海外陆架线状沙脊群精细结构及其成因机制项目
    (40506017); 大洋DY115-20南海综合海试航次联合资助

Abstract:

The study area of this paper is the slope of the Shenhu Area in the northern South China Sea. We interpreted both sub-bottom and single-channel seismic profiles to describe the acoustic characteristics of gas hydrate sediment and to discuss the cause of its formation. We distinguished some abnormal physiognomy and geologic objects that are relevantrelative to gas hydrate in profiles. Protuberance, shallow fault, acoustic blank patch, partial enhanced reflection and acoustic blank zone were discovered in the legible sub-bottom profile. The shallow gassy belt locates under the seabed from 34 to 82m. Contrasting the sub-bottom profile with the data of China’s first gas hydrate expedition, we believed that the gas in the shallow gassy belt came from the decompounding of deeper gas hydrate. Pockmark, seepage, drape and Bottom Simulating Reflector(BSR)were recognized in the single-channel seismic profile. The depth of BSR is slightly deeper than that for the sample of China’s first gas hydrate expedition in the study area. The BSR in the seismic profile might be the bottom of gas hydrate. Based on the time-depth conversion, we plotted out Oligocene, early Miocene epoch, middle Miocene epoch and Pliocene in the seismic profile according to the sediment depth, sediment speed and age of ODP1148 and set up the chronology of the gas hydrate sediment.

Key words: north slope of South China Sea, Shenhu Sea Area, gas hydrate, sub-bottom profile, single-channel seismic profile, chronology