1Woodside J M, Ivanov M K, Limonov A F. Neotectonics and fluid flow through seafloor sediments in the Eastern Mediterranean and Black Seas-Parts I and II[C]. IOC Tech. Ser. ,1997,48.
2Vogt P R, Gardner J, Crane K. The Norwegian-BarentsSvalbard (NBS) continental margin: Introducing a natural laboratory of mass wasting, hydrates, and ascent of sediment[J]. Geo-Mar. Lett., 1999,19:2-21.
3Ginsburg G D. Gas hydrate accumulation at the Hakon Mosby mud volcanoe[J]. Geo-Marine Letters, 1999,19:57-67.
4Martin J B, Kastner M, Henry P,et al. Chemical and isotopic evidence for sources of fluid in a mud volcano field seaward of the Barbados accretionary wedge [J]. J. Geophys. Res. ,1996,101:20 325-20 345.
5Heggland R, Nygaard E, Gallagher J W. Techniques and experiences using exploration 3D seismic data to map drilling Hazards[A]. Offshore Technology Conference[C]. Houston, TX, 1996. 119-127.
6Corthay II J E. Delineation of a massive seafloor hydrocarbon seep, overpressured aquifer sands, and shallow gas reservoir,Louisiana continental slope[A]. Offshore Technology Conference[C]. Houston, Texas, 1998.37-56.
7Yin P, Berne S, Vagner P,et al. Mud volcanoes at the shelf margin of the East China Sea[J]. Marine Geology, 2003(194): 135-149.
8Kvenvolden K A. Natural gas hydrate occurrence and issues[A]. International Conference on Natural Gas Hydrates[C].Plenum Press, 1995. 233-246.
9Rao Y H,Subrahmanyam C. Slope failures along the western continentsl margin of India:a consequense of gas hydrate dissociation,rapid sedimentation rate and seismic activity? [J].Marine Letters,2002,22(3):162-169.
10Stoll R D,Ewing J I,Bryan G M. Anomalous wave velocities in sediments containing gas hydrates[J]. Journal of Geophysical Research, 1971,76:2 090-2 094.
