南海北部深水盆地流体活动系统及其成藏意义
|
摘要
根据高精度的3D和2D地震资料,对南海北部深水盆地的流体活动系统的类型、影响因素和它们之间的演化关系进行了研究.南海北部深水区存在着包括:泥火山、泥底辟、气烟囱、管状通道、多边形断层和构造断层等多种类型的流体活动系统.根据地震反射特征,可以把它们划分为断层有关的流体活动系统和柱状流体活动系统两大类.研究发现研究区内的流体活动系统主要受构造和沉积两方面的影响.并且,气烟囱、泥底辟和泥火山存在着单向演化的关系,可以从是否有沉积物参与运移及是否喷出海底将它们区分开来.最后,本文探讨了流体活动系统对深水油气和天然气水合物成藏的重要影响,建立了南海北部流体活动系统的存在模式.
The types,influencing factors and their evolutions of focused fluid flow systems in the northern South China Sea(SCS)are deeply studied based on high-resolution 3Dand 2Dseismic data.These systems include mud volcanoes,mud diapirs,gas chimneys,pipes,polygonal faults and tectonic faults.They are influenced by both tectonism and sedimentation.The gas chimneys,mud diapirs and mud volcanoes may have relationship of unidirectional evolution and we can separate them from whether the sediments are involved and whether the sediments or fluids erupt into the seawater or not.Finally,a development model of focused fluid flow systems in the northern SCS is proposed.Because their great importance for the deep-water resource exploration(hydrocarbon and gas hydrate),they should receive much attention from now on.
The types,influencing factors and their evolutions of focused fluid flow systems in the northern South China Sea(SCS)are deeply studied based on high-resolution 3Dand 2Dseismic data.These systems include mud volcanoes,mud diapirs,gas chimneys,pipes,polygonal faults and tectonic faults.They are influenced by both tectonism and sedimentation.The gas chimneys,mud diapirs and mud volcanoes may have relationship of unidirectional evolution and we can separate them from whether the sediments are involved and whether the sediments or fluids erupt into the seawater or not.Finally,a development model of focused fluid flow systems in the northern SCS is proposed.Because their great importance for the deep-water resource exploration(hydrocarbon and gas hydrate),they should receive much attention from now on.
引文
Boetius A,Ravenschlag K,Schubert C J,et al.2000.A marinemicrobial consortium apparently mediating anaerobic oxidationof methane.Nature,407(6804):623-626,doi:10.1038/35036572.
Cartwright J A.1994.Episodic basin-wide hydrofracturing ofoverpressured early Cenozoic mudrock sequences in the NorthSea Basin.Mar.Petrol.Geol.,11(5):587-607,doi:10.1016/0264-8172(94)90070-1.
Cartwright J A.2011.Diagenetically induced shear failure of finegrained sediments and the development of polygonal faultsystems.Mar.Petrol.Geol.,28(9):1593-1610,doi:10.1016/j.marpetgeo.2011.06.004.
Cartwright J A,Huuse M,Aplin A.2007.Seal bypass systems.AAPG Bull.,91(8):1141-1166,doi:10.1306/04090705181.
Cathles L M,Su Z,Chen D F.2010.The physics of gas chimneyand pockmark formation,with implications for assessment ofseafloor hazards and gas sequestration.Mar.Petrol.Geol.,27(1):82-91,doi:10.1016/j.marpetgeo.2009.09.010.
Chen D F,Li X X,Xia B.2004.Distribution of gas hydrate stablezones and resource prediction in the Qiongdongnan Basin of theSouth China Sea.Chinese J.Geophys.(in Chinese),47(3):483-489,doi:10.3321/j.issn:0001-5733.2004.03.018.
Chen D F,Huang Y Y,Yuan X L,et al.2005.Seep carbonates andpreserved methane oxidizing Archaea and sulfate reducingbacteria fossils suggest recent gas venting on the seafloor in thenortheastern South China Sea.Mar.Petrol.Geol.,22(5):613-621,doi:10.1016/j.marpetgeo.2005.05.002.
Chen D X.,Wu S G,Wang X J,et al.2011.Seismic expression ofpolygonal faults and its impact on fluid flow migration for gashydrates formation in deep water of the South China Sea.Journal of Geological Research,2011:384785,doi:10.1155/2011/384785.
Dimitrov L I.2003.Mud volcanoes—a significant source ofatmospheric methane.Geo-Mar.Lett.,23(3-4):155-161,doi:10.1007/s00367-003-0140-3.
Dong D D.2008.The geological evolution and resource in the deepwater area of northern South China Sea(in Chinese)[Ph.D.thesis].Beijing:Graduate University of Chinese AcademySciences.
Hao F,Dong W L,Zou H Y,et al.2003.Overpressure fluid flowand rapid accumulation of natural gas in Yinggehai Basin.ActaPetrolei Sinica(in Chinese),24(6):7-12.
He J X,Yan W,Ma W H,et al.2010a.The geological significanceof the paragenetic association of hydrocarbon and hydrate inQuasi-passive margin the northern South China Sea.JournalofSouthwest Petroleum University(Science&TechnologyEdition)(in Chinese),32(6):5-10.
He J X,Zhu Y H,Weng R N,et al.2010b.Characters of northwest mud diapirs volcanoes in South China Sea and relationshipbetween them and accumulation and migration of oil and gas.Earth Science(Journal of China University of Geosciences)(inChinese),35(1):75-86.
Hedberg H D.1974.Relation of methane generation toundercompacted shales,shale diapirs,and mud volcanoes.AAPG Bull.,58(4):661-673.
Huuse M,Jackson A L C,Van Rensbergen P,et al.2010.Subsurface sediment remobilization and fluid flow in sedimentarybasins:an overview.Basin Res.,22(4):342-360,doi:10.1111/j.1365-2117.2010.00487.x.
Judd A G,Hovland M.2007.Seabed Fluid Flow:The Impact onGeology,Biology,and the Marine Environment.Cambridge:Cambridge University Press.
Kopf A.2002.Significance of mud volcanism.Rev.Geophys.,40(2):2-1-2-52,doi:10.1029/2000RG000093.
Kopf A,Delisle G,Faber E,et al.2010.Long-term in situmonitoring at Dashgil mud volcano,Azerbaijan:a link betweenseismicity,pore-pressure transients and methane emission.Int.J.Earth Sci.,99(1):227-240,doi:10.1007/s00531-009-0487-4.
Kopf A,Klaeschen D,Mascle J.2001.Extreme efficiency of mudvolcanism in dewatering accretionary prisms.Earth Planet.Sci.Lett.,189(3-4):295-313,doi:10.1016/S0012-821X(01)00278-3.
Lavrushin V U,Polyak B G,Prasolov R M,et al.1996.Sources ofmaterial in mud volcano products(based on isotopic,hydrochemical,and geological data).Lith.Min.Res.,31(6):557-578.
Lüdmann T,Wong H K.1999.Neotectonic regime on the passivecontinental margin of the northern South China Sea.Tectonophysics,311(1-4):113-138,doi:10.1016/S0040-1951(99)00155-9.
L seth H,Gading M,Wensaas L.2009.Hydrocarbon leakageinterpreted on seismic data.Mar.Petrol.Geol.,26(7):1304-1319,doi:10.1016/j.marpetgeo.2008.09.008.
L seth H,Wensaas L,Arntsen B,et al.2011.1000 mlong gasblow-out pipes.Mar.Petrol.Geol.,28(5):1047-1060,doi:10.1016/j.marpetgeo.2010.10.001.
Milkov A V.2000.Worldwide distribution of submarine mudvolcanoes and associated gas hydrates.Mar.Geol.,167(1-2):29-42,doi:10.1016/S0025-3227(00)00022-0.
Orange D L,Teas P A,Decker J,et al.2008.The utilisation ofSeaSeep surveys(a defense/hydrography spin-off)to identifyand sample hydrocarbon seeps in offshore frontier basins.//International Petroleum Technology Conference.Kuala Lumpur.
Sun Q L.2011.Focused fluid flow escape systems and soft sedimentdeformations in the deep-water basins,northern South ChinaSea(in Chinese)[Ph.D.thesis].Beijing:Graduate Universityof Chinese Academy of Sciences.
Sun Q L,Cartwright J,Wu S G,et al.2013b.3D seismicinterpretation of dissolution pipes in the South China Sea:Genesis by subsurface,fluid induced collapse.Mar.Geol.,337:171-181,doi:10.1016/j.margeo.2013.03.002.
Sun Q L,Wu S G,Cartwright J A,et al.2012a.Shallow gas andfocused fluid flow systems in the Pearl River Mouth Basin,northern South China Sea.Mar.Geol.,315-318:1-14,doi:10.1016/j.margeo.2012.05.003.
Sun Q L,Wu S G,Cartwright J A,et al.2013a.Focused fluid flowsystems of the Zhongjiannan Basin and Guangle Uplift,SouthChina Sea.Basin Res.,25(1):97-111,doi:10.1111/j.1365-2117.2012.00551.x.
Sun Y B,Wu S G,Dong D D,et al.2012b.Gas hydrates associatedwith gas chimneys in fine-grained sediments of the northernSouth China Sea.Mar.Geol.,311-314:32-40,doi:10.1016/j.margeo.2012.04.003.
Sun Q L,Wu S G,Hovland M,et al.2011.The morphologies andgenesis of mega-pockmarks near the Xisha Uplift,South ChinaSea.Mar.Petrol.Geol.,28(6):1146-1156,doi:10.1016/j.marpetgeo.2011.03.003.
Sun Q L,Wu S G,LüF L,et al.2010.Polygonal faults and theirimplications for hydrocarbon reservoirs in the southernQiongdongnan Basin,South China Sea.J.Asian Earth Sci.,39(5):470-479,doi:10.1016/j.jseaes.2010.04.002.
Sun Q L,Wu S G,Yao G S,et al.2009.Characteristics andFormation Mechanism of Polygonal Faults in QiongdongnanBasin,Northern South China Sea.J.Earth Sci.,20(1):180-192,doi:10.1007/s12583-009-0018-z.
Wang D W,Wu S G,Qin Z L,et al.2009.Architecture andidentification of large Quaternary mass transport depositions inthe slope of South China Sea.Marine Geology&QuaternaryGeology(in Chinese),29(5):65-72.
Wang J H,Pang X,Wang C W,et al.2006.Discovery andrecognition of the central diapiric zone in Baiyun Depression,Pearl River Mouth Basin.Earth Science(Journal of ChinaUniversity of Geosciences)(in Chinese),31(2):209-213.
Wang X J,Hutchinson D R,Wu S G,et al.2011.Elevated gashydrate saturation within silt and silty clay sediments in theShenhu area,South China Sea.J.Geophys.Res.:Solid Earth(1978—2012),116(B5):B05102,doi:10.1029/2010JB007944.
Wu N Y,Yang S X,Wang H B,et al.2009.Gas-bearing fluidinflux sub-system for gas hydrate geological system in ShenhuArea,Northern South China Sea.Chinese J.Geophys.(inChinese),52(6):1641-1650,doi:10.3969/j.issn.0001-5733.2009.06.027.
Wu S G,Han Q H,Ma Y B,et al.2009.Petroleum System inDeepwater Basins of the Northern South China Sea.J.EarthSci.,20(1):124-135,doi:10.1007/s12583-009-0014-3.
Wu S G,Sun Q L,Wu T Y,et al.2009.Polygonal fault and oil-gasaccumulation in deep-water area of Qiongdongnan Basin.ActaPetrolet Sinica(in Chinese),30(1):22-26.
Xie X N,Jiang T,Wang H,et al.2006a.Expulsion ofoverpressured fluid revealed by geochemistry of formation waterin the dirpiric structures of Yinggehai basin.Acta PetrologicaSinica(in Chinese),22(8):2243-2248.
Xie X N,Müller R D,Li S T,et al.2006b.Origin of anomaloussubsidence along the Northern South China Sea margin and itsrelationship to dynamic topography.Mar.Petrol.Geol.,23(7):745-765,doi:10.1016/j.marpetgeo.2006.03.004.
Yassir N A.1989.Mud volcanoes and the behaviour of overpressured claysand silts[Ph.D.thesis].London:University College London.
Zhang G C,Mi L J,Wu S G,et al.2007.Deepwater area—the newprospecting targets of northern continental margin of SouthChina Sea.Acta Petrolet Sinica(in Chinese),28(2):15-21.
Zhao S J,Wu S G,Shi H S,et al.2012.Structures and dynamicmechanism related to the Dongsha Movement at the northernmargin of South China Sea.Progress in Geophysics(inChinese),27(3):1008-1019.
Zhu W L,Huang B J,Mi L J,et al.2009.Geochemistry,origin,and deep-water exploration potential of natural gases in thePearl River Mouth and Qiongdongnan basins,South China Sea.AAPG Bull.,93(6):741-761,doi:10.1306/02170908099.
Zhu W L,Zhang G C,Yang S K,et al.2007.Gas Geology innorthern continental margin of South China Sea(in Chinese).Beijing:Petroleum Industry Press.
陈多福,李绪宣,夏斌.2004.南海琼东南盆地天然气水合物稳定域分布特征及资源预测.地球物理学报,47(3):483-489.
董冬冬.2008.南海北部陆缘深水区构造演化及其资源效应[博士论文].北京:中国科学院研究生院(海洋研究所).
郝芳,董伟良,邹华耀等.2003.莺歌海盆地汇聚型超压流体流动及天然气晚期快速成藏.石油学报,24(6):7-12
何家雄,颜文,马文宏等.2010a.南海准被动陆缘深水油气与水合物共生意义.西南石油大学学报(自然科学版),32(6):5-10.
何家雄,祝有海,翁荣南等.2010b.南海北部边缘盆地泥底辟及泥火山特征及其与油气运聚关系.地球科学(中国地质大学学报),35(1):75-86.
孙启良.2011.南海北部深水盆地流体逸散系统与沉积物变形[博士论文].北京:中国科学院研究生院(海洋研究所).
王大伟,吴时国,秦志亮等.2009.南海陆坡大型块体搬运体系的结构与识别特征.海洋地质与第四纪地质,29(5):65-72.
王家豪,庞雄,王存武等.2006.珠江口盆地白云凹陷中央底辟带的发现及识别.地球科学(中国地质大学学报),31(2):209-213.
吴能友,杨胜雄,王宏斌等.2009.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.地球物理学报,52(6):1641-1650.
吴时国,孙启良,吴拓宇等.2009.琼东南盆地深水区多边形断层的发现及其油气意义.石油学报,30(1):22-26.
解习农,江涛,王华等.2006.莺歌海盆地底辟带热流体突破的地层水化学证据.岩石学报,22(8):2243-2248.
张功成,米立军,吴时国等.2007.深水区—南海北部大陆边缘盆地油气勘探新领域.石油学报,28(2):15-21.
赵淑娟,吴时国,施和生等.2012.南海北部东沙运动的构造特征及动力学机制探讨.地球物理学进展,27(3):1008-1019.
朱伟林,张功成,杨少坤等.2007.南海北部大陆边缘盆地天然气地质.北京:石油工业出版社.
Cartwright J A.1994.Episodic basin-wide hydrofracturing ofoverpressured early Cenozoic mudrock sequences in the NorthSea Basin.Mar.Petrol.Geol.,11(5):587-607,doi:10.1016/0264-8172(94)90070-1.
Cartwright J A.2011.Diagenetically induced shear failure of finegrained sediments and the development of polygonal faultsystems.Mar.Petrol.Geol.,28(9):1593-1610,doi:10.1016/j.marpetgeo.2011.06.004.
Cartwright J A,Huuse M,Aplin A.2007.Seal bypass systems.AAPG Bull.,91(8):1141-1166,doi:10.1306/04090705181.
Cathles L M,Su Z,Chen D F.2010.The physics of gas chimneyand pockmark formation,with implications for assessment ofseafloor hazards and gas sequestration.Mar.Petrol.Geol.,27(1):82-91,doi:10.1016/j.marpetgeo.2009.09.010.
Chen D F,Li X X,Xia B.2004.Distribution of gas hydrate stablezones and resource prediction in the Qiongdongnan Basin of theSouth China Sea.Chinese J.Geophys.(in Chinese),47(3):483-489,doi:10.3321/j.issn:0001-5733.2004.03.018.
Chen D F,Huang Y Y,Yuan X L,et al.2005.Seep carbonates andpreserved methane oxidizing Archaea and sulfate reducingbacteria fossils suggest recent gas venting on the seafloor in thenortheastern South China Sea.Mar.Petrol.Geol.,22(5):613-621,doi:10.1016/j.marpetgeo.2005.05.002.
Chen D X.,Wu S G,Wang X J,et al.2011.Seismic expression ofpolygonal faults and its impact on fluid flow migration for gashydrates formation in deep water of the South China Sea.Journal of Geological Research,2011:384785,doi:10.1155/2011/384785.
Dimitrov L I.2003.Mud volcanoes—a significant source ofatmospheric methane.Geo-Mar.Lett.,23(3-4):155-161,doi:10.1007/s00367-003-0140-3.
Dong D D.2008.The geological evolution and resource in the deepwater area of northern South China Sea(in Chinese)[Ph.D.thesis].Beijing:Graduate University of Chinese AcademySciences.
Hao F,Dong W L,Zou H Y,et al.2003.Overpressure fluid flowand rapid accumulation of natural gas in Yinggehai Basin.ActaPetrolei Sinica(in Chinese),24(6):7-12.
He J X,Yan W,Ma W H,et al.2010a.The geological significanceof the paragenetic association of hydrocarbon and hydrate inQuasi-passive margin the northern South China Sea.JournalofSouthwest Petroleum University(Science&TechnologyEdition)(in Chinese),32(6):5-10.
He J X,Zhu Y H,Weng R N,et al.2010b.Characters of northwest mud diapirs volcanoes in South China Sea and relationshipbetween them and accumulation and migration of oil and gas.Earth Science(Journal of China University of Geosciences)(inChinese),35(1):75-86.
Hedberg H D.1974.Relation of methane generation toundercompacted shales,shale diapirs,and mud volcanoes.AAPG Bull.,58(4):661-673.
Huuse M,Jackson A L C,Van Rensbergen P,et al.2010.Subsurface sediment remobilization and fluid flow in sedimentarybasins:an overview.Basin Res.,22(4):342-360,doi:10.1111/j.1365-2117.2010.00487.x.
Judd A G,Hovland M.2007.Seabed Fluid Flow:The Impact onGeology,Biology,and the Marine Environment.Cambridge:Cambridge University Press.
Kopf A.2002.Significance of mud volcanism.Rev.Geophys.,40(2):2-1-2-52,doi:10.1029/2000RG000093.
Kopf A,Delisle G,Faber E,et al.2010.Long-term in situmonitoring at Dashgil mud volcano,Azerbaijan:a link betweenseismicity,pore-pressure transients and methane emission.Int.J.Earth Sci.,99(1):227-240,doi:10.1007/s00531-009-0487-4.
Kopf A,Klaeschen D,Mascle J.2001.Extreme efficiency of mudvolcanism in dewatering accretionary prisms.Earth Planet.Sci.Lett.,189(3-4):295-313,doi:10.1016/S0012-821X(01)00278-3.
Lavrushin V U,Polyak B G,Prasolov R M,et al.1996.Sources ofmaterial in mud volcano products(based on isotopic,hydrochemical,and geological data).Lith.Min.Res.,31(6):557-578.
Lüdmann T,Wong H K.1999.Neotectonic regime on the passivecontinental margin of the northern South China Sea.Tectonophysics,311(1-4):113-138,doi:10.1016/S0040-1951(99)00155-9.
L seth H,Gading M,Wensaas L.2009.Hydrocarbon leakageinterpreted on seismic data.Mar.Petrol.Geol.,26(7):1304-1319,doi:10.1016/j.marpetgeo.2008.09.008.
L seth H,Wensaas L,Arntsen B,et al.2011.1000 mlong gasblow-out pipes.Mar.Petrol.Geol.,28(5):1047-1060,doi:10.1016/j.marpetgeo.2010.10.001.
Milkov A V.2000.Worldwide distribution of submarine mudvolcanoes and associated gas hydrates.Mar.Geol.,167(1-2):29-42,doi:10.1016/S0025-3227(00)00022-0.
Orange D L,Teas P A,Decker J,et al.2008.The utilisation ofSeaSeep surveys(a defense/hydrography spin-off)to identifyand sample hydrocarbon seeps in offshore frontier basins.//International Petroleum Technology Conference.Kuala Lumpur.
Sun Q L.2011.Focused fluid flow escape systems and soft sedimentdeformations in the deep-water basins,northern South ChinaSea(in Chinese)[Ph.D.thesis].Beijing:Graduate Universityof Chinese Academy of Sciences.
Sun Q L,Cartwright J,Wu S G,et al.2013b.3D seismicinterpretation of dissolution pipes in the South China Sea:Genesis by subsurface,fluid induced collapse.Mar.Geol.,337:171-181,doi:10.1016/j.margeo.2013.03.002.
Sun Q L,Wu S G,Cartwright J A,et al.2012a.Shallow gas andfocused fluid flow systems in the Pearl River Mouth Basin,northern South China Sea.Mar.Geol.,315-318:1-14,doi:10.1016/j.margeo.2012.05.003.
Sun Q L,Wu S G,Cartwright J A,et al.2013a.Focused fluid flowsystems of the Zhongjiannan Basin and Guangle Uplift,SouthChina Sea.Basin Res.,25(1):97-111,doi:10.1111/j.1365-2117.2012.00551.x.
Sun Y B,Wu S G,Dong D D,et al.2012b.Gas hydrates associatedwith gas chimneys in fine-grained sediments of the northernSouth China Sea.Mar.Geol.,311-314:32-40,doi:10.1016/j.margeo.2012.04.003.
Sun Q L,Wu S G,Hovland M,et al.2011.The morphologies andgenesis of mega-pockmarks near the Xisha Uplift,South ChinaSea.Mar.Petrol.Geol.,28(6):1146-1156,doi:10.1016/j.marpetgeo.2011.03.003.
Sun Q L,Wu S G,LüF L,et al.2010.Polygonal faults and theirimplications for hydrocarbon reservoirs in the southernQiongdongnan Basin,South China Sea.J.Asian Earth Sci.,39(5):470-479,doi:10.1016/j.jseaes.2010.04.002.
Sun Q L,Wu S G,Yao G S,et al.2009.Characteristics andFormation Mechanism of Polygonal Faults in QiongdongnanBasin,Northern South China Sea.J.Earth Sci.,20(1):180-192,doi:10.1007/s12583-009-0018-z.
Wang D W,Wu S G,Qin Z L,et al.2009.Architecture andidentification of large Quaternary mass transport depositions inthe slope of South China Sea.Marine Geology&QuaternaryGeology(in Chinese),29(5):65-72.
Wang J H,Pang X,Wang C W,et al.2006.Discovery andrecognition of the central diapiric zone in Baiyun Depression,Pearl River Mouth Basin.Earth Science(Journal of ChinaUniversity of Geosciences)(in Chinese),31(2):209-213.
Wang X J,Hutchinson D R,Wu S G,et al.2011.Elevated gashydrate saturation within silt and silty clay sediments in theShenhu area,South China Sea.J.Geophys.Res.:Solid Earth(1978—2012),116(B5):B05102,doi:10.1029/2010JB007944.
Wu N Y,Yang S X,Wang H B,et al.2009.Gas-bearing fluidinflux sub-system for gas hydrate geological system in ShenhuArea,Northern South China Sea.Chinese J.Geophys.(inChinese),52(6):1641-1650,doi:10.3969/j.issn.0001-5733.2009.06.027.
Wu S G,Han Q H,Ma Y B,et al.2009.Petroleum System inDeepwater Basins of the Northern South China Sea.J.EarthSci.,20(1):124-135,doi:10.1007/s12583-009-0014-3.
Wu S G,Sun Q L,Wu T Y,et al.2009.Polygonal fault and oil-gasaccumulation in deep-water area of Qiongdongnan Basin.ActaPetrolet Sinica(in Chinese),30(1):22-26.
Xie X N,Jiang T,Wang H,et al.2006a.Expulsion ofoverpressured fluid revealed by geochemistry of formation waterin the dirpiric structures of Yinggehai basin.Acta PetrologicaSinica(in Chinese),22(8):2243-2248.
Xie X N,Müller R D,Li S T,et al.2006b.Origin of anomaloussubsidence along the Northern South China Sea margin and itsrelationship to dynamic topography.Mar.Petrol.Geol.,23(7):745-765,doi:10.1016/j.marpetgeo.2006.03.004.
Yassir N A.1989.Mud volcanoes and the behaviour of overpressured claysand silts[Ph.D.thesis].London:University College London.
Zhang G C,Mi L J,Wu S G,et al.2007.Deepwater area—the newprospecting targets of northern continental margin of SouthChina Sea.Acta Petrolet Sinica(in Chinese),28(2):15-21.
Zhao S J,Wu S G,Shi H S,et al.2012.Structures and dynamicmechanism related to the Dongsha Movement at the northernmargin of South China Sea.Progress in Geophysics(inChinese),27(3):1008-1019.
Zhu W L,Huang B J,Mi L J,et al.2009.Geochemistry,origin,and deep-water exploration potential of natural gases in thePearl River Mouth and Qiongdongnan basins,South China Sea.AAPG Bull.,93(6):741-761,doi:10.1306/02170908099.
Zhu W L,Zhang G C,Yang S K,et al.2007.Gas Geology innorthern continental margin of South China Sea(in Chinese).Beijing:Petroleum Industry Press.
陈多福,李绪宣,夏斌.2004.南海琼东南盆地天然气水合物稳定域分布特征及资源预测.地球物理学报,47(3):483-489.
董冬冬.2008.南海北部陆缘深水区构造演化及其资源效应[博士论文].北京:中国科学院研究生院(海洋研究所).
郝芳,董伟良,邹华耀等.2003.莺歌海盆地汇聚型超压流体流动及天然气晚期快速成藏.石油学报,24(6):7-12
何家雄,颜文,马文宏等.2010a.南海准被动陆缘深水油气与水合物共生意义.西南石油大学学报(自然科学版),32(6):5-10.
何家雄,祝有海,翁荣南等.2010b.南海北部边缘盆地泥底辟及泥火山特征及其与油气运聚关系.地球科学(中国地质大学学报),35(1):75-86.
孙启良.2011.南海北部深水盆地流体逸散系统与沉积物变形[博士论文].北京:中国科学院研究生院(海洋研究所).
王大伟,吴时国,秦志亮等.2009.南海陆坡大型块体搬运体系的结构与识别特征.海洋地质与第四纪地质,29(5):65-72.
王家豪,庞雄,王存武等.2006.珠江口盆地白云凹陷中央底辟带的发现及识别.地球科学(中国地质大学学报),31(2):209-213.
吴能友,杨胜雄,王宏斌等.2009.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.地球物理学报,52(6):1641-1650.
吴时国,孙启良,吴拓宇等.2009.琼东南盆地深水区多边形断层的发现及其油气意义.石油学报,30(1):22-26.
解习农,江涛,王华等.2006.莺歌海盆地底辟带热流体突破的地层水化学证据.岩石学报,22(8):2243-2248.
张功成,米立军,吴时国等.2007.深水区—南海北部大陆边缘盆地油气勘探新领域.石油学报,28(2):15-21.
赵淑娟,吴时国,施和生等.2012.南海北部东沙运动的构造特征及动力学机制探讨.地球物理学进展,27(3):1008-1019.
朱伟林,张功成,杨少坤等.2007.南海北部大陆边缘盆地天然气地质.北京:石油工业出版社.
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心