[1] Max M D. Natural gas hydrate in oceanic and permafrost
environments[M]. Dordrecht：Kluwer Academic Publishers，
2003.
[2] Sloan E D. Clathrate hydrate of natural gases [M]. 2nd ed.
New York：Marcel Dekker，1998.
[3] Paull C K，Buelow W J，Ussler W，et al. Increased
continental-margin slumping frequency during sea-level
lowstands above gas hydrate-bearing sediments[J]. Geology，
1996，24（2）：143 146.
[4] Rothwell R G，Thomson J，Kähler G. Low-sealevel
emplacement of a very large Late Pleistocene
‘megaturbidite’in the western Mediterranean Sea[J].
Nature，1998，392（6674）：377 380.
[5] Mienert J，Vanneste M，Bünz S，et al. Ocean warming and
gas hydrate stability on the mid-norwegian margin at the
Storegga Slide[J]. Marine and Petroleum Geology，2005，
22（1）：233 244.
[6] Dillon W P，Nealon J W，Taylor M H，et al. Seafloor collapse
and methane venting associated with gas hydrate on
the blake ridge：causes and implications to seafloor stability
and methanerelease[M]//Paull C K，Dillon W P. Natural
Gas Hydrates：Occurrence，Distribution，and Detection.
Washington DC，American：American Geophysical
Union，2001：211 233.
[7] Vogt P R， Gardner J， Crane K. The Norwegian
Barents Svalbard（NBS） continental margin：
introducing a natural laboratory of mass wasting，
hydrates，and ascent of sediment，pore water，and
methane[J]. Geo-Marine Letters，1999，19（1 2）：2 21.
[8] Van Rensbergen P，De Batist M，Klerkx J，et al. Sublacustrine
mud volcanoes and methane seeps caused by dissociation
of gas hydrates in Lake Baikal[J]. Geology，2002，
30（7）：631 634.
[9] Zühlsdorff L，Spiess V. Three-dimensional seismic characterization
of a venting site reveals compelling indications
of natural hydraulic fracturing[J]. Geology，2004，
32（2）：101 104.
[10] Kennett J P，Fackler-Adams B N. Relationship of clathrate
instability to sediment deformation in the upper Neogene
of California[J]. Geology，2000，28（3）：215 218.
[11] Davies R，Cartwright J，Rana J. Giant hummocks in deepwater
marine sediments：Evidence for large-scale differential
compaction and density inversion during early buri
al[J]. Geology，1999，27（10）：907 910.
[12] Kennett J P，Cannariato K G，Hendy I L，et al. Methane
hydrates in quaternary climate change：The clathrate gun
hypothesis[M]. Washington D C：AGU，2003.
[13] Grozic J L H，Kvalstad T J. Effect of gas on deepwater marine
sediments[C]//Proceedings of The International Conference
on Soil Mechanics and Geotechnical Engineering.
Aa Balkema Publishers，2001，3：2289 2294.
[14] Flemings P B，Liu X，Winters W J. Critical pressure and
multiphase flow in Blake Ridge gas hydrates[J]. Geology，
2003，31（12）：1057 1060.
[15] Sultan N，Cochonat P，Foucher J P，et al. Effect of gas
hydrates melting on seafloor slope instability[J]. Marine
Geology，2004，213（1）：379 401.
[16] Xu W，Germanovich L N. Excess pore pressure resulting
from methane hydrate dissociation in marine sediments：A
theoretical approach[J]. Journal of Geophysical Research，
2006，111（B1）：1 12.
[17] Wroth C P. Correlations of some engineering properties
of soils[C]//Proceedings of the Second International Conference
on the Behaviour of Off-Shore Structures，held at
Imperial College，London，England，1979.
[18] Nixon M F. Influence of gas hydrates on submarine slope
stability[D]. Albert：University of Calagary，2005.
[19] 杨晓云. 天然气水合物与海底滑坡研究[D]. 北京：中国
石油大学，2010.