[1] MAX M D.Natural gas hydrate in oceanic and permafrost environments[M]. Switzerland: Springer Science & Business Media, 2003, 432. DOI: 10.1007/978-94-011-4387-5.
[2] VADAKKEPULIYAMBATTA S, BÜNZ S, MIENERT J, et al. Distribution of subsurface fluid-flow systems in the SW Barents Sea[J]. Marine and Petroleum Geology, 2013, 43: 208-221. DOI: 10.1016/j.marpetgeo.2013.02.007.
[3] LABERG J S, ANDREASSEN K, KNUTSEN S M.Inferred gas hydrate on the Barents Sea shelf-a model for its formation and a volume estimate[J]. Geo-marine letters, 1998, 18(1): 26-33. DOI: 10.1007/s003670050048.
[4] ANDREASSEN K, HOGSTAD K, BERTEUSSEN K A.Gas hydrate in the southern Barents Sea, indicated by a shallow seismic anomaly[J]. First break, 1990, 8(6): 235-245. DOI: 10.3997/1365-2397.1990012.
[5] 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. DOI: 10.1007/s003670050088.
[6] PAULL C, DALLIMORE S, HUGHES-CLARKE J, et al.Tracking the decomposition of submarine permafrost and gas hydrate under the shelf and slope of the Beaufort Sea[C]//7th International Conference on Gas Hydrates. Shell, Edinburgh, UK, 2011.
[7] PAULL C K, DALLIMORE S R, HUGHES CLARKE J E, et al. Active seafloor gas vents on the Shelf and upper Slope in Canadian Beaufort Sea[C]//Presented at the Fall Meeting of the American Geophysical Union. San Francisco, California: American Geophysical Union, 2012.
[8] VADAKKEPULIYAMBATTA S, HORNBACH M J, BÜNZ S, et al. Controls on gas hydrate system evolution in a region of active fluid flow in the SW Barents Sea[J]. Marine and petroleum geology, 2015, 66: 861-872. DOI: 10.1016/j.marpetgeo.2015.07.023.
[9] MIENERT J, POSEWANG J.Evidence of shallow- and deep-water gas hydrate destabilizations in North Atlantic polar continental margin sediments[J]. Geo-marine letters, 1999, 19(1/2): 143-149. DOI: 10.1007/s003670050101.
[10] MIENERT J, BÜNZ S, GUIDARD S, et al. Ocean bottom seismometer investigations in the Ormen Lange area offshore mid-Norway provide evidence for shallow gas layers in subsurface sediments[J]. Marine and petroleum geology, 2005, 22(1/2): 287-297. DOI: 10.1016/j.marpetgeo.2004.10.020.
[11] CHAND S, MIENERT J, ANDREASSEN K, et al.Gas hydrate stability zone modelling in areas of salt tectonics and pockmarks of the Barents Sea suggests an active hydrocarbon venting system[J]. Marine and petroleum geology, 2008, 25(7): 625-636. DOI: 10.1016/j.marpetgeo. 2007.10.006.
[12] MILLER J J, LEE M W, VON HUENE R.An Analysis of a Seismic Reflection from the Base of a Gas Hydrate Zone, Offshore Peru[J]. AAPG bulletin, 1991, 75(5): 910-924.
[13] ANDREASSEN K, HART P E, MACKAY M.Amplitude versus offset modeling of the bottom simulating reflection associated with submarine gas hydrates[J]. Marine geology, 1997, 137(1/2): 25-40. DOI: 10.1016/S0025-3227(96)00076-X.
[14] ANDREASSEN K, HANSEN T.Inferred gas hydrates offshore Norway and Svalbard[J]. Norsk geologisk tidsskrift, 1995, 45: 10-34.
[15] GABRIELSEN R H, FÆRSETH R B, JENSEN L N, et al. Structural elements of the Norwegian continental shelf, part I: the Barents Sea region[J]. NPD bulletin 1990, 6: 45.
[16] CHAND S, THORSNES T, RISE L, et al. Multiple episodes of fluid flow in the SW Barents Sea (Loppa High) evidenced by gas flares, pockmarks and gas hydrate accumulation[J]. Earth and planetary science letters, 2012, 331-332: 305-314. DOI: 10.1016/j.epsl.2012.03.021.
[17] OSTANIN I, ANKA Z, DI PRIMIO R, et al. Identification of a large Upper Cretaceous polygonal fault network in the Hammerfest basin: Implications on the reactivation of regional faulting and gas leakage dynamics, SW Barents Sea[J]. Marine geology, 2012, 332-334: 109-125. DOI: 10.1016/j.margeo.2012.03.005.
[18] NICKEL J C, DI PRIMIO R, MANGELSDORF K, et al. Characterization of microbial activity in pockmark fields of the SW-Barents Sea[J]. Marine geology, 2012, 332-334: 152-162. DOI: 10.1016/j.margeo.2012.02.002.
[19] HOVLAND M, JUDD A G.Seabed pockmarks and seepages: impact on geology, biology and marine environment[M]. London: Graham and Trotman, 1988.
[20] OSTANIN I, ANKA Z, DI PRIMIO R, et al.Hydrocarbon plumbing systems above the Snøhvit gas field: structural control and implications for thermogenic methane leakage in the Hammerfest Basin, SW Barents Sea[J]. Marine and petroleum geology, 2013, 43: 127-146. DOI: 10.1016/j.marpetgeo.2013.02.012.
[21] BJORØY M, HALL P B, FERRIDAY I L, et al. Triassic source rocks of the Barents Sea and Svalbard[J]. Search and discovery, 2010, 10219: 7.
[22] CARTWRIGHT J.The impact of 3D seismic data on the understanding of compaction, fluid flow and diagenesis in sedimentary basins[J]. Journal of the geological society, 2007, 164(5): 881-893. DOI: 10.1144/0016-76492006-143.
[23] DORÉ A G.Barents Sea geology, petroleum resources and commercial potential[J]. Arctic, 1995, 48(3): 207-221. DOI: 10.14430/arctic1243.
[24] CARTWRIGHT J, HUUSE M, APLIN A.Seal bypass systems[J]. AAPG bulletin, 2007, 91(8): 1141-1166. DOI: 10.1306/04090705181.
[25] OHM S E, KARLSEN D A, AUSTIN T J F. Geochemically driven exploration models in uplifted areas: Examples from the Norwegian Barents Sea[J]. AAPG bulletin, 2008, 92(9): 1191-1223. DOI: 10.1306/06180808028.
[26] GUDLAUGSSON S T, FALEIDE J I, JOHANSEN S E, et al.Late Palaeozoic structural development of the South-western Barents Sea[J]. Marine and petroleum geology, 1998, 15(1): 73-102. DOI: 10.1016/S0264-8172(97)00048-2.
[27] WORSLEY D.The post-Caledonian development of Svalbard and the western Barents Sea[J]. Polar research, 2008, 27(3): 298-317. DOI: 10.1111/j.1751-8369.2008. 00085.x.
[28] SMELROR M, PETROV O V, LARSSEN G B, et al.Geological history of the Barents Sea[M]. Trondheim, Norway: NGU, 2009.
[29] JOHANSEN S E, OSTISTY B K, BIRKELAND Ø, et al.Hydrocarbon potential in the Barents Sea region: play distribution and potential[M]//VORREN T O, BERGSAGER E, DAHL-STAMNES Ø A, et al. Arctic Geology and Petroleum Potential. Amsterdam: Elsevier, 1993: 273-320. DOI: 10.1016/B978-0-444-88943-0.50024-1.
[30] BREKKE H, RIIS F.Mesozoic tectonics and basin evolution of the Norwegian Shelf between 60°N and 72°N[J]. Norsk geologisk tidsskrift, 1987, 67: 295-322.
[31] RIIS F, VOLLSET J, SAND M.Tectonic development of the western margin of the Barents Sea and adjacent areas[J]//HALBOUTY M T. Future Petroleum Provinces of the World. AAPG, 1986: 661-676.
[32] ZIEGLER P A.Evolution of the Arctic-North Atlantic and the Western Tethys[M]. Tulsa, Oklahoma, U.S.A: AAPG, 1988: 198.
[33] FALEIDE J I, VÅGNES E, GUDLAUGSSON S T. Late Mesozoic-Cenozoic evolution of the south-western Barents Sea in a regional rift-shear tectonic setting[J]. Marine and petroleum geology, 1993, 10(3): 186-214. DOI: 10.1016/0264-8172(93)90104-Z.
[34] ELDHOLM O, FALEIDE J I, MYHRE A M. Continent- ocean transition at the western Barents Sea/Svalbard continental margin[J]. Geology, 1987, 15(12): 1118-1122. DOI: 10.1130/0091-7613(1987)15<1118:CTATWB>2.0.CO;2.
[35] FALEIDE J I, SOLHEIM A, FIEDLER A, et al.Late Cenozoic evolution of the western Barents Sea-Svalbard continental margin[J]. Global and planetary change, 1996, 12(1/4): 53-74. DOI: 10.1016/0921-8181(95)00012-7.
[36] TALWANI M, ELDHOLM O. Evolution of the Norwegian- Greenland Sea[J]. GSA bulletin, 1977, 88(7): 969-999. DOI: 10.1130/0016-7606(1977)88<969:EOTNS>2.0.CO;2.
[37] MYHRE A M, ELDHOLM O, SUNDVOR E.The margin between Senja and Spitsbergen fracture zones: Implications from plate tectonics[J]. Tectonophysics, 1982, 89(1/3): 33-50. DOI: 10.1016/0040-1951(82)90033-6.
[38] VORREN T O, RICHARDSEN G, KNUTSEN S M, et al.Cenozoic erosion and sedimentation in the western Barents Sea[J]. Marine and petroleum geology, 1991, 8(3): 317-340. DOI: 10.1016/0264-8172(91)90086-G.
[39] SOLHEIM A, KRISTOFFERSEN Y.Sediments above the upper regional unconformity: thickness, seismic stratigraphy and outline of the glacial history[M]. Norsk Polarinst Skr, 1984, 179B: 26.
[40] EIDVIN T, JANSEN E, RIIS F.Chronology of Tertiary fan deposits off the western Barents Sea: implications for the uplift and erosion history of the Barents Shelf[J]. Marine geology, 1993, 112(1/4): 109-131. DOI: 10.1016/0025-3227(93)90164-Q.
[41] ANDREASSEN K, LABERG J S, VORREN T O.Seafloor geomorphology of the SW Barents Sea and its glaci- dynamic implications[J]. Geomorphology, 2008, 97(1/2): 157-177. DOI: 10.1016/j.geomorph.2007.02.050.
[42] FALEIDE J I, TSIKALAS F, BREIVIK A J, et al.Structure and evolution of the continental margin off Norway and the Barents Sea[J]. Episodes, 2008, 31(1): 82-91.
[43] TASIANAS A, BÜNZ S, BELLWALD B, et al. High-resolution 3D seismic study of pockmarks and shallow fluid flow systems at the Snøhvit hydrocarbon field in the SW Barents Sea[J]. Marine geology, 2018, 403: 247-261. DOI: 10.1016/j.margeo.2018.06.012.
[44] OSTANIN I, ANKA Z, DI PRIMIO R.Role of faults in Hydrocarbon leakage in the Hammerfest Basin, SW Barents Sea: insights from seismic data and numerical modelling[J]. Geosciences, 2017, 7(28): 30. DOI: 10.3390/geosciences7020028.
[45] MURILLO W A, VIETH-HILLEBRAND A, HORSFIELD B, et al.Petroleum source, maturity, alteration and mixing in the southwestern Barents Sea: New insights from geochemical and isotope data[J]. Marine and petroleum geology, 2016, 70: 119-143. DOI: 10.1016/j.marpetgeo.2015.11.009.
[46] Collett T S.Gas Hydrate Petroleum Systems in Marine and Arctic Permafrost Environments[J]. GCSSEPM Proceedings, 2009: 6-30. DOI: 10.5724/gcs.09.29.0006.
