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AVO Character Research of Natural Gas Hydrates in the East China Sea 被引量:1

AVO Character Research of Natural Gas Hydrates in the East China Sea
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摘要 Natural gas hydrates are considered as strategic resources with commercial potential in the 21st century. Obvious BSR characteristics will be shown on seismic profiles, if there exist natural gas hydrates. The AVO method is one of the methods which can be used to identify and forecast lithologic characteristics and fluid properties by using the relationship between Amplitude and Offset. AVO anomaly is one of the significant signs to check out whether or not there is free gas below the BSR, so it can be used to detect natural gas hydrates from the seismic profile. Considering the geological and geophysical characteristics of the Okinawa Trough and making use of the techniques mentioned above, we can conclude that the conditions there are favorable for the formation and concentration of natural gas hydrates. By analyzing the data collected from the study area, one can discover many different anomalous phenomena on the seismic profile which are related to the existence of natural gas hydrates. Preliminary estimation of the natural gas hydrates in the Okinawa Trough shows that the trough is rich in natural gas hydrates and may become a potential important resources exploration area. Natural gas hydrates are considered as strategic resources with commercial potential in the 21st century. Obvious BSR characteristics will be shown on seismic profiles, if there exist natural gas hydrates. The AVO method is one of the methods which can be used to identify and forecast lithologic characteristics and fluid properties by using the relationship between Amplitude and Offset. AVO anomaly is one of the significant signs to check out whether or not there is free gas below the BSR, so it can be used to detect natural gas hydrates from the seismic profile. Considering the geological and geophysical characteristics of the Okinawa Trough and making use of the techniques mentioned above, we can conclude that the conditions there are favorable for the formation and concentration of natural gas hydrates. By analyzing the data collected from the study area, one can discover many different anomalous phenomena on the seismic profile which are related to the existence of natural gas hydrates. Preliminary estimation of the natural gas hydrates in the Okinawa Trough shows that the trough is rich in natural gas hydrates and may become a potential important resources exploration area.
出处 《Journal of Ocean University of China》 SCIE CAS 2009年第3期270-276,共7页 中国海洋大学学报(英文版)
基金 supported by the National High Technology Research and Development (863) Program (Grant No.2006AA09Z339) the Natural Science Foundation of Shandong, China (Grant No. Y2006E09)
关键词 natural gas hydrates free gas blank zone Okinawa Trough 天然气水合物 AVO异常 海洋法 中国 特性 地震剖面 地球物理特征 战略资源
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  • 1Geertsma J,Smit D C,1961.Some aspects of elastic wave propagation in fluid-saturated porous solids.Geophysics,26:169-181
  • 2Hyndman R,Spence G,1992.A seismic study of methane hydrates marine bottom simulating reflectors.J Geophys Res,97:6683-6698
  • 3Kvenvolden K A,1993.Gas hydrate-geological perspective and global change.Rev Geophys,31(2):173-187
  • 4Matsumoto R,Uchida T,Waseda A et al,2000.Occurrence,structure and composition of natural gas hydrate recovered from the Blake Ridge,Northwest Atlantic.Paull C K,Matsumoto R,Wallace P J et al ed.Proceedings of the Ocean Drilling Program,Scientific Results,164:13-28
  • 5Minshull T A,Singh S C,Westbrook G K,1994.Seismic velocity structure at a gas hydrate reflector,offshore western Columbia,from full waveform inversion.J Geophys Res,99:4715-4734
  • 6Ostrander W J,1984.Plane-wave reflection coefficients for gas sand at normal angles of incidence.Geophysics,49:1637-1649
  • 7Sloan E D,1990.Clathrate hydrates of natural gas.New York:Marcel Deffer Inc,1-641
  • 8Tinivella U,Accaino F,2000.Compressional-wave velocity structure and Poisson's ratio in marine sediments with gas hydrate and free gas by inversion of reflection of reflected and refracted seismic data(South Shetland Islands,Antarctica).Marine Geol,164:13-27
  • 9Tinivella U,2002.The seismic response to overpressure versus gas hydrate and free gas concentration.J Seismic Expl,11:283-305
  • 10Zoeppritz K,1919.Erdbebenwellen Ⅷ b:ber Reflexionen und Durchgang seismischer Wellen durch Unstetigkeits-flchen.Gttinger Nachrichten,1:66-84

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