引文
[1]Stoll R D,Ewing J I,Bryan G M.Anomalous wave velocities insediments containing gas hydrate[J].Journal of GeophysicalResearch,1971,76:2090-2094.
[2]Ewing J I,Hollister C H.Regional aspects of deep sea drilling inthe western North Atlantic[CD-ROM].Initial Reports,DeepSea Drilling Project 11,1972:951-973.
[3]Tobin HJ,Moore J C,Mackay M E,et al.Fluid-flow along astrike-slip-fault at the toe of the Oregon accretionary prism—Im-plications for the geometry of frontal accretion[J].GeologicalSociety of America Bulletin,1993,105(5):569-582.
[4]Zuhlsdorff L,Spiess V,Hubscher C,et al.Implications for fo-cused fluid transport at the northern Cascadia accretionary prismfrom a correlation between BSR occurrence and near-sea-floor re-flectivity anomalies imaged in a multi-frequency seismic data set[J].International Journal of Earth Sciences,2000,88(4):655-667.
[5]Delisle G,Berner U.Gas hydrates acting as cap rock to fluiddischarge in the Makran accretionary prism[J].Tectonic andClimatic Evolution of the Arabian Sea Region,2002,195:137-146.
[6]Moore G F,Taira A,Klaus A,et al.Newinsights into deforma-tion and fluid flow processes in the Nankai Trough accretionaryprism:Results of Ocean Drilling Program Leg 190[J].Geo-chemistry,Geophysics,Geosystems,2001,2(10):1058,doi:10.1029/2001GC000166.
[7]Baba K,Yamada Y.BSRs and associated reflections as an indi-cator of gas hydrate and free gas accumulation:An example of ac-cretionary prism and forearc basin system along the NankaiTrough,off Central Japan[J].Resource Geology,2004,54(1):11-24.
[8]Ghosh R,Sain K.Effective medium modeling to assess gas hy-drate and free-gas evident from the velocity structure in the Mak-ran accretionary prism,offshore Pakistan[J].Marine Geophysi-cal Researches,2008,29(4):267-274.
[9]丁巍伟,程晓敢,陈汉林,等.台湾增生楔的构造单元划分及其变形特征[J].热带海洋学报,2005,24(5):53-59.
[10]许升辉,阎贫,刘海龄.台湾西南海域似海底反射分析[J].热带海洋学报,2005,24(2):79-85.
[11]宋海斌,吴时国,江为为.南海东北部973剖面BSR及其热流特征[J].地球物理学报,2007,50(5):1508-1517.
[12]黄慈流,钟建强.南海东北部及其邻区新生代构造事件[J].热带海洋,1994,13(1):55-62.
[13]姚伯初,万玲,吴能友.大南海地区新生代板块构造活动[J].中国地质,2004,31(2):113-122.
[14]McDonnell S L,Max MD,Cherkis N Z,et al.Tectono-sedi-mentary controls on the likelihood of gas hydrate occurrence nearTaiwan[J].Marine and PetroleumGeology,2000,17(8):929-936.
[15]李家彪,金翔龙,阮爱国,等.马尼拉海沟增生楔中段的挤入构造[J].科学通报,2004,49(10):1000-1008.
[16]Hirtzel J,Chi W C,Reed D.Destruction of Luzon forearc basinfrom subduction to Taiwan arc-continent collision[J].Tectono-physics,2009,479:43-51.
[17]姚伯初.南海天然气水合物的形成和分布[J].海洋地质与第四纪地质,2005,25(2):81-90.
[18]Liu C S,Schnurle P,Wang Y.Distribution and characters of gashydrate offshore of southwestern Taiwan[J].Terrestrial,Atmos-pheric and Oceanic Sciences,2006,17(4):615-644.
[19]Huang C Y,Chien C W,Zhao M,et al.Geological study of ac-tive cold seeps in the syn-collision accretionary prism Kaopingslope off SW Taiwan[J].Terrestrial,Atmospheric and OceanicSciences,2006,17(4):679-702.
[20]Yan P,Deng H,Liu HL.The geological structure and prospectof gas hydrate over the Dongsha slope,South China Sea[J].Terrestrial,Atmospheric and Oceanic Sciences,2006,17(4):645-658.
[21]Claypool G E,Kvenvolden K A.Methane and other hydrocarbongases in marine sediments[J].Annual Review of Earth andPlanetary Sciences,1983,11(1):299-327.
[22]Kvenvolden K A.A review of the geochemistry of methane innatural gas hydrate[J].Organic Geochemistry,1995,23:177-189.
[23]樊栓狮,刘锋,陈多福.海洋天然气水合物的形成机理探讨[J].天然气地球科学,2004,15(5):524-530.
[24]吴时国,姚根顺,董冬冬,等.南海北部陆坡大型气田区天然气水合物的成藏地质构造特征[J].石油学报,2008,29(3):324-328.
[25]陆红锋,刘坚,陈芳,等.南海台西南区碳酸盐岩矿物学和稳定同位素组成特征——天然气水合物存在的主要证据之一[J].地学前缘,2005,12(3):268-276.
[26]Hyndman R D,Davis E E.A mechanism for the formation ofmethane hydrate and seafloor bottom-simulating reflectors by verti-cal fluid expulsion[J].Journal of Geophysics Research—SolidEarth,1992,97(B5):7025-7041.
[27]Wang P,Prell W L,Blum P,et al.Proceeding of the OceanDrilling Program[CD-ROM].Initial Reports,184:CollegeStation,TX:Ocean Drilling Program,2000.
[28]栾锡武,翟世奎,干晓群.冲绳海槽中部热液活动区构造地球物理特征分析[J].沉积学报,2001,19(1):43-47.
[29]龚跃华,杨胜雄,王宏斌,等.南海北部神狐海域天然气水合物成藏特征[J].现代地质,2009,23(2):210-216.
[30]浦晓强,陶小晚,张会领.南海北部陆坡天然气水合物存在的地球物理和地球化学特征[J].天然气地球科学,2009,20(4):620-626.
[31]金庆涣,张光学,杨木壮,等.天然气水合物资源概论[M].北京:科学出版社,2006:108-109.
[32]姚伯初,杨木壮.南海晚新生代构造运动与天然气水合物资源[J].海洋地质与第四纪地质,2008,28(4):93-100.
[33]方银霞,高金耀,黎明碧,等.冲绳海槽天然气水合物与地质构造的关系[J].海洋地质与第四纪地质,2005,25(1):85-91.
[34]Milkov A V.Worldwide distribution of submarine mud volcanoesand associated gas hydrate[J].Marine Geology,2000,167(1/2):29-42.
[35]Chiu J K,Tseng W H,Liu C S.Distribution of gassy sedimentsand mud volcanoes offshore southwestern Taiwan[J].Terrestri-al,Atmospheric and Oceanic Sciences,2006,17(4):703-722.
[36]Milkov AV,Sassen R.Economic geology of offshore gas hydrateaccumulations and provinces[J].Marine and Petroleum Geolo-gy,2002,19(1):1-11.
[37]Yan P,Berne S,Vagner P,et al.Mud volcanoes at the shelfmargin of the East China Sea[J].Marine Geology,2003,194:135-149.
[38]王宏语,孙春岩,张洪波,等.西沙海槽潜在天然气水合物成因及形成地质模式[J].海洋地质与第四纪地质,2005,25(4):85-91.
[39]吴能友,杨胜雄,王宏斌,等.南海北部陆坡神狐海域天然气水合物成藏的流体运移体系[J].地球物理学报,2009,52(6):1641-1650.
[40]Wessel P,Smith W H F.New version of the generic mappingtools(GMT)version3.0 released[J].Trans AGUEOS,1995,76:329.