南海南部陆缘礼乐盆地新生代的构造-沉积特征及伸展机制:来自NH973-2多道地震测线的证据
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摘要
针对"973"项目中"南海大陆边缘动力学与油气资源潜力"这一研究课题,对在南海南部陆缘礼乐盆地采集的NH973-2测线进行了研究.对地震剖面的解释共划分出6个层序界面,将地层划分为4个构造沉积单元.根据地震解释,对不同时期断层的水平断距进行了测量及分析,获取了与脆性拉张相关的伸展信息:研究区的拉张作用可以分为2期,主要的拉张作用发生在大陆裂谷阶段(古近纪),形成了一系列的地堑-半地堑以及翘倾断块;第2期拉张作用的时期为晚渐新世-早中新世,断层活动强度明显变弱.在南海南部陆缘广泛发育了碳酸盐沉积,其发育的时代和南海的海底扩张时期一致.对穿越礼乐滩区地震剖面伸展特征的分析表明,根据断层水平断距获得脆性伸展因子与根据重力反演获得的全地壳伸展因子之间存在差异,表明研究区的拉张在纵向上并非是均一的,新生代的拉张经历了深度决定拉张模式.
One recently acquired regional multi-channel seismic profile(NH973-2) across the Reed Bank basin,the South China Sea(SCS),is interpreted.Based on the interpretations of these profiles,we have worked out its stratigraphic sequences,tectonic structures and extension factors.Four tectonic-stratigraphic units are determined,together with 6 sequence boundaries.Detailed analyses on the extension factors based on the measurement of fault heaves reveal two episodes of continental extension separated by a distinct unconformity.The main extension occurred during the continental rifting(Early Tertiary),and resulted in the formation of half-grabens and rotated blocks,controlled by deeply rooted detachment system.During the second extension phase(drifting period,Late Oligocene-Early Miocene) intensity reduced sharply and focused on the continental-oceanic transition area.A widespread carbonate platform developed across the Reed bank region concurrent with the drifting period of the SCS.Fault-related stretching factor(βf) is found to be comparable and shows discrepancy with the whole crust stretching factors(βc) in the study area.Thus we conclude that the continental crust of the Reed Bank basin experienced depth-dependent extension.
One recently acquired regional multi-channel seismic profile(NH973-2) across the Reed Bank basin,the South China Sea(SCS),is interpreted.Based on the interpretations of these profiles,we have worked out its stratigraphic sequences,tectonic structures and extension factors.Four tectonic-stratigraphic units are determined,together with 6 sequence boundaries.Detailed analyses on the extension factors based on the measurement of fault heaves reveal two episodes of continental extension separated by a distinct unconformity.The main extension occurred during the continental rifting(Early Tertiary),and resulted in the formation of half-grabens and rotated blocks,controlled by deeply rooted detachment system.During the second extension phase(drifting period,Late Oligocene-Early Miocene) intensity reduced sharply and focused on the continental-oceanic transition area.A widespread carbonate platform developed across the Reed bank region concurrent with the drifting period of the SCS.Fault-related stretching factor(βf) is found to be comparable and shows discrepancy with the whole crust stretching factors(βc) in the study area.Thus we conclude that the continental crust of the Reed Bank basin experienced depth-dependent extension.
引文
Barckhausen,U.,Roeser,H.A.,2004.Seafloor spreadinganomalies in the South China Sea revisited.In:Clift,P.D.,Wang,P.X.,Kuhnt,W.,eds.,continent-ocean interactionswithin the East Asian marginal seas.Geophysical Monograph,AGU,Washington,D.C.,149:121-125.
Briais,A.,Patriat,P.,Tapponnier,P.,1993.Updated interpretation of magnetic anomalies and seafloor spreading stages inthe South China Sea:implications for the Tertiary tectonicsof Southeast Asia.Journal of Geophysical Research,98(B4):6299-6328.doi:10.1029/92JB02280
Chen,Y.L.,Niu,F.L.,Liu,R.F.,et al.,2010.Crustalstructure beneath China from receiver function analysis.Journal of Geophysical Research,115:B03307.doi:10.1029/2009JB006386
Clift,P.,Lee,G.H.,Anh Duc,N.,et al.,2008.Seismic reflection evidence for a dangerous grounds miniplate:noextrusion origin for the South China Sea.Tectonics,27(3):TC3008.doi:10.1029/2007TC002216
Clift,P.,Lin,J.,2001.Preferential mantle lithospheric extensionunder the South China margin.Mar.Petrol.Geol.,18(8):929-945.doi:10.1016/S02648172(01)00037-x
Contrucci,I.,Matias,L.,Moulin,M.,et al.,2004.Deep structure of the West African continental margin(Congo,Zaire,Angola),between5°S and8°S,from reflection/refractionseismics and gravity data.Geophys.J.Int.,158:529553.doi:10.1111/j.1365-246X.2004.02303.x
Crosby,A.G.,White,N.J.,Edwards,G.R.H.,et al.,2011.Evolution of deep-water rifted margins:testingdepth-dependent extensional models.Tectonics,30:TC1004.doi:10.1029/2010TC002687
Davis,M.,Kusznir,N.J.,2003.Depth-dependent lithophericstretching at rifted continental margin.In:Karner,G.D.,ed.,Proceedings of NSF Rifted Margins.ColumbiaUniversity Press,New York,92-136.
Driscoll,N.W.,Karner,G.D.,1998.Lower crustal extension across the northern Carnarvon basin,Australia:evidence for an eastward dipping detachment.Journal ofGeophysical Research,103(B3):4975-4991.doi:10.1029/97JB03295
Franke,D.,Barckhausen,U.,Baristeas,N.,et al.,2011,Thecontinent-ocean transition at the southeastern margin ofthe South China Sea.Mar.Petrol.Geol.,28(6):11871204.doi:10.1016/j.marpetgeo.2011.01.004
Franke,D.,Barckhausen,U.,Heyde,I.,et al.,2008.Seismicimages of a collision zone offshore NW Sabah/Borneo.Mar.Petrol.Geol.,25(7):606-624.doi:10.1016/j.marpetgeo.2007.11.004
Fuller,M.,Ali,J.R.,Moss,S.J.,et al.,1999.Paleomagnetism of borneo.J.Asian.Earth.Sci.,17(1-2):324.doi:10.1016/S07439547(98)00057-9
Gao,H.F.,Zeng,X.H.,Liu,Z.H.,et al.,2005.Simulatingof subsidence history and analysis of tectonic evolutionary characteristics of Liyue basin in South China Sea.Geotectonica et Metallogenia,29(3):385-390(in Chinese with English abstract).
Hinz,K.,Fritsch,J.,Kempter,E.H.K.,et al.,1989.Thrust tectonics along the continental margin of Sabah/Borneo.Geologische Rundschau,78(3):705-730.doi:10.1007/BF01829317
Hinz,K.,Schlueter,H.U.,1985.Geology of the dangerousgrounds,South China Sea,and the continental margin off Southwest Palawan:results of SONNE Cruises SO23and SO-27.Energy,10(3-4):297-315.doi:10.1016/0360-5442(85)90048-9
Holloway,N.H.,1982.North Palawan block,Philippines:its relation to Asian mainland and role in evolution ofSouth China Sea.AAPG Bull.,66(9):1355-1383.
Holt,R.A.,1998.The gravity field of Sundaland:acquisition,assessment and interpretation(Disertation).University of London,London.
Hutchison,C.S.,2004.Marginal basin evolution:the southern South China Sea.Mar.Petrol.Geol.,21(9):11291148.doi:10.1016/j.marpetgeo.2004.07.002
Hutchison,E.S.,2005.Geology of North-West Borneo:Sarawak,Brunei and Sabah.Elsevier,Amsterdam.
Kudrass,H.R.,Wiedicke,M.,Cepek,P.,et al.,1986.Mesozoicand Cainozoic rocks dredged from the South China Sea(Reed Bank area)and Sulu Sea and their significance forplate-tectonic reconstructions.Mar.Petrol.Geol.,3(1):19-30.doi:10.1016/0264-8172(86)90053-X
Kusznir,N.J.,Hunsdale,R.,Roberts,A.M.,et al.,2005.Norwegian margin depth-dependent stretching,In:Doré,A.G.,Vining,B.A.,Davies,R.J.,eds.,Petroleum geology:North-west Europe and global perspectives-proceedings of the6th petroleum geology conference.Geological Society.,London,767-783.
Li,J.B.,2008.Evolution of China's marginal seas and itseffect of natural resources.Ocean Press,Beijing(in Chinese).
Luedmann,T.,Wong,H.K.,1999.Neotectonic regime onthe passive continental margin of the northern SouthChina Sea.Tectonophysics,311(1-4):113-138.doi:10.1016/S0040-1951(99)00155-9
McKenzie,D.,1978.Some remarks on the development ofsedimentary basins.Earth and Planetary Science Letter,40:25-32.
Meredith,D.J.,Egan,S.S.,2002.The geological and geodynamic evolution of the eastern Black Sea basin:insights from2D and3-D tectonic modelling.Tectonophysics,350(2):151-179.doi:10.1016/S0040-1951(02)0012-X
Morley,C.K.,2002.A tectonic model for the Tertiary evolution of strike-slip faults and rift basins in SE Asia.Tectonophysics,347(4):189-215.doi:10.1016/S00401951(02)00061-6
Northrup,C.J.,Royden,L.H.,Brurchfiel,B.C.,1995.Motionof the Pacific plate relativn to Eurasia and its potential relation to Cenozoic extension along the eastern margin of Eurasia.Geology,23(8):719-722.doi:10.1130/0091-7613(1995)023<0719:MOTPPR>203.CO;2
Reston,T.,2005.Polyphase faulting during the developmentof the West Galicia rifted margin.Earth and PlanetaryScience Letter,237:561-576.doi:10.1016/j.epsl.2005.06.019
Reston,T.,2009.Extension discrepancy at North Atlanticnonvolcanic rifted margins:depth-dependent stretchingor unrecognized faulting?Geology,35(4):367-370.doi:10.1130/G23213A.1
Sales,A.O.,Jacobsen,E.C.,Morado,J.A.A.,et al.,1997.Thepetroleum potential of deep-water Northwest Palawan blockGSEC66.Journal of Asian Earth Sciences,15(2):217240.doi:10.1016/S1367-9120(97)00009-6
Schlueter,H.U.,Hinz,K.,Block,M.,1996.Tectono-stratigraphic terranes and detachment faulting of the SouthChina Sea and Sulu Sea.Mar.Geol.,130(1-2):3978.doi:10.1016/0025-3227(95)00137-9
Shipboard Scientific Party,2000.Leg184summary:exploring the Asian monsoon through drilling in the SouthChina Sea,In:Wang,P.,Prell,W.L.,Blum,P.,et al.,eds.,Proc.ODP,initial results.184:college station,TX(ocean drilling program),1-77.doi:10.2973/odp.proc.ir.184.101.2000
Sibuet,J.C.,1992.New constraints on the formation of thenon-volcanic continental Galicia-Flemish Cap conjugatemargins.Journal of the Ceological Society,149(5):829-840.doi:10.1144/gsgs.149.5.0829
Sun,L.T.,Sun,Z.,Zhan,W.H.,et al.,2010.Petroleum potential prediction of the Lile basin in Nansha.Earth Science—Journal of China University of Geosciences,35(1):137-145(in Chinese with English abstract).
Sun,L.T.,Sun,Z.,Zhou,D.,et al.,2008.Stratigraphic andstructural characteristics of Lile basin in Nansha area.Geotectonica et Metallogenia,32(2):151-158(in Chinese with English abstract).
Sun,Z.,Zhong,Z.H.,Keep,M.,et al.,2009.3Danaloguemodeling of the South China Sea:a discussion onbreakup pattern.J.Asian.Earth.Sci.,34(4):544556.doi:10.1016/j.jseaes.2008.09.002
Taylor,B.,Hayes,D.E.,1983.Origin and history of theSouth China Sea basin.In:Hayes,D.E.,ed.,The tectonic and geologic evolution of the Southeast Asian seasand islands.Part2,Geophys.Monogr.,AGU,Washington,D.C.,23-56.
Whitmarsh,R.B.,Manatschal,G.,Minshull,T.A.,2001.Evolution of magma-poor continental margins from rifting to seafloor spreading.Nature,413:150-154.doi:10.1038/35093085
Williams,H.H.,1997.Play concepts—northwest Palawan,Philippines.J.Asian.Earth.Sci.,15(2-3):251273.doi:10.1016/S0743-9547(97)00011-1
Yan,P.,Liu,H.L.,2004.Tectonic-stratigraphic division andblind fold structures in Nansha waters,South ChinaSea.J.Asian.Earth.Sci.,24:337-348.
Yao,B.C.,Zeng,W.J.,Hayes,D.E.,1994.The geologicalmemoir of South China Sea surveyed by jointly China&U.S.A..China University of Geosciences Press,Wuhan(in Chinese).
Zhang,L.,Li,W.C.,Zeng,X.H.,2003.Stratigraphic sequence and hydrocarbon potential in Lile basin.Petroleum Geology&Experiment,25(5):469-480(in Chinese with English abstract).
Zhou,D.,Ru,K.,Chen,H.Z.,1995.Kinematics of Cenozoicextension on the South China Sea continental marginand its implications for the tectonic evolution of the region.Tectonophysics,251(1-4):161-177.doi:10.1016/0040.1951(95)00018-6
Ziegler,P.A.,1983.Crustal thinning and subsidence in theNorth Sea.Nature,304(5926):561.doi:10.1038/304561a0
高红芳,曾祥辉,刘振湖,等,2005.南海礼乐盆地沉降史模拟及构造演化特征分析.大地构造与成矿学,29(3):385-390.
李家彪,2008.中国边缘海形成演化与资源效应.北京:海洋出版社.
孙龙涛,孙珍,詹文欢,等,2010.南沙海域礼乐盆地油气资源潜力.地球科学——中国地质大学学报,35(1):137-145.
孙龙涛,孙珍,周蒂,等,2008.南沙海区礼乐盆地沉积地层与构造特征分析.大地构造与成矿学,32(2):151-158.
姚伯初,曾维军,Hayes,D.E.,1994.中美合作调研南海地质专报.武汉:中国地质大学出版社.
张莉,李文成,曾祥辉,2003.礼乐盆地地层发育特征及其与油气的关系.石油实验地质,25(5):469-480.
Briais,A.,Patriat,P.,Tapponnier,P.,1993.Updated interpretation of magnetic anomalies and seafloor spreading stages inthe South China Sea:implications for the Tertiary tectonicsof Southeast Asia.Journal of Geophysical Research,98(B4):6299-6328.doi:10.1029/92JB02280
Chen,Y.L.,Niu,F.L.,Liu,R.F.,et al.,2010.Crustalstructure beneath China from receiver function analysis.Journal of Geophysical Research,115:B03307.doi:10.1029/2009JB006386
Clift,P.,Lee,G.H.,Anh Duc,N.,et al.,2008.Seismic reflection evidence for a dangerous grounds miniplate:noextrusion origin for the South China Sea.Tectonics,27(3):TC3008.doi:10.1029/2007TC002216
Clift,P.,Lin,J.,2001.Preferential mantle lithospheric extensionunder the South China margin.Mar.Petrol.Geol.,18(8):929-945.doi:10.1016/S02648172(01)00037-x
Contrucci,I.,Matias,L.,Moulin,M.,et al.,2004.Deep structure of the West African continental margin(Congo,Zaire,Angola),between5°S and8°S,from reflection/refractionseismics and gravity data.Geophys.J.Int.,158:529553.doi:10.1111/j.1365-246X.2004.02303.x
Crosby,A.G.,White,N.J.,Edwards,G.R.H.,et al.,2011.Evolution of deep-water rifted margins:testingdepth-dependent extensional models.Tectonics,30:TC1004.doi:10.1029/2010TC002687
Davis,M.,Kusznir,N.J.,2003.Depth-dependent lithophericstretching at rifted continental margin.In:Karner,G.D.,ed.,Proceedings of NSF Rifted Margins.ColumbiaUniversity Press,New York,92-136.
Driscoll,N.W.,Karner,G.D.,1998.Lower crustal extension across the northern Carnarvon basin,Australia:evidence for an eastward dipping detachment.Journal ofGeophysical Research,103(B3):4975-4991.doi:10.1029/97JB03295
Franke,D.,Barckhausen,U.,Baristeas,N.,et al.,2011,Thecontinent-ocean transition at the southeastern margin ofthe South China Sea.Mar.Petrol.Geol.,28(6):11871204.doi:10.1016/j.marpetgeo.2011.01.004
Franke,D.,Barckhausen,U.,Heyde,I.,et al.,2008.Seismicimages of a collision zone offshore NW Sabah/Borneo.Mar.Petrol.Geol.,25(7):606-624.doi:10.1016/j.marpetgeo.2007.11.004
Fuller,M.,Ali,J.R.,Moss,S.J.,et al.,1999.Paleomagnetism of borneo.J.Asian.Earth.Sci.,17(1-2):324.doi:10.1016/S07439547(98)00057-9
Gao,H.F.,Zeng,X.H.,Liu,Z.H.,et al.,2005.Simulatingof subsidence history and analysis of tectonic evolutionary characteristics of Liyue basin in South China Sea.Geotectonica et Metallogenia,29(3):385-390(in Chinese with English abstract).
Hinz,K.,Fritsch,J.,Kempter,E.H.K.,et al.,1989.Thrust tectonics along the continental margin of Sabah/Borneo.Geologische Rundschau,78(3):705-730.doi:10.1007/BF01829317
Hinz,K.,Schlueter,H.U.,1985.Geology of the dangerousgrounds,South China Sea,and the continental margin off Southwest Palawan:results of SONNE Cruises SO23and SO-27.Energy,10(3-4):297-315.doi:10.1016/0360-5442(85)90048-9
Holloway,N.H.,1982.North Palawan block,Philippines:its relation to Asian mainland and role in evolution ofSouth China Sea.AAPG Bull.,66(9):1355-1383.
Holt,R.A.,1998.The gravity field of Sundaland:acquisition,assessment and interpretation(Disertation).University of London,London.
Hutchison,C.S.,2004.Marginal basin evolution:the southern South China Sea.Mar.Petrol.Geol.,21(9):11291148.doi:10.1016/j.marpetgeo.2004.07.002
Hutchison,E.S.,2005.Geology of North-West Borneo:Sarawak,Brunei and Sabah.Elsevier,Amsterdam.
Kudrass,H.R.,Wiedicke,M.,Cepek,P.,et al.,1986.Mesozoicand Cainozoic rocks dredged from the South China Sea(Reed Bank area)and Sulu Sea and their significance forplate-tectonic reconstructions.Mar.Petrol.Geol.,3(1):19-30.doi:10.1016/0264-8172(86)90053-X
Kusznir,N.J.,Hunsdale,R.,Roberts,A.M.,et al.,2005.Norwegian margin depth-dependent stretching,In:Doré,A.G.,Vining,B.A.,Davies,R.J.,eds.,Petroleum geology:North-west Europe and global perspectives-proceedings of the6th petroleum geology conference.Geological Society.,London,767-783.
Li,J.B.,2008.Evolution of China's marginal seas and itseffect of natural resources.Ocean Press,Beijing(in Chinese).
Luedmann,T.,Wong,H.K.,1999.Neotectonic regime onthe passive continental margin of the northern SouthChina Sea.Tectonophysics,311(1-4):113-138.doi:10.1016/S0040-1951(99)00155-9
McKenzie,D.,1978.Some remarks on the development ofsedimentary basins.Earth and Planetary Science Letter,40:25-32.
Meredith,D.J.,Egan,S.S.,2002.The geological and geodynamic evolution of the eastern Black Sea basin:insights from2D and3-D tectonic modelling.Tectonophysics,350(2):151-179.doi:10.1016/S0040-1951(02)0012-X
Morley,C.K.,2002.A tectonic model for the Tertiary evolution of strike-slip faults and rift basins in SE Asia.Tectonophysics,347(4):189-215.doi:10.1016/S00401951(02)00061-6
Northrup,C.J.,Royden,L.H.,Brurchfiel,B.C.,1995.Motionof the Pacific plate relativn to Eurasia and its potential relation to Cenozoic extension along the eastern margin of Eurasia.Geology,23(8):719-722.doi:10.1130/0091-7613(1995)023<0719:MOTPPR>203.CO;2
Reston,T.,2005.Polyphase faulting during the developmentof the West Galicia rifted margin.Earth and PlanetaryScience Letter,237:561-576.doi:10.1016/j.epsl.2005.06.019
Reston,T.,2009.Extension discrepancy at North Atlanticnonvolcanic rifted margins:depth-dependent stretchingor unrecognized faulting?Geology,35(4):367-370.doi:10.1130/G23213A.1
Sales,A.O.,Jacobsen,E.C.,Morado,J.A.A.,et al.,1997.Thepetroleum potential of deep-water Northwest Palawan blockGSEC66.Journal of Asian Earth Sciences,15(2):217240.doi:10.1016/S1367-9120(97)00009-6
Schlueter,H.U.,Hinz,K.,Block,M.,1996.Tectono-stratigraphic terranes and detachment faulting of the SouthChina Sea and Sulu Sea.Mar.Geol.,130(1-2):3978.doi:10.1016/0025-3227(95)00137-9
Shipboard Scientific Party,2000.Leg184summary:exploring the Asian monsoon through drilling in the SouthChina Sea,In:Wang,P.,Prell,W.L.,Blum,P.,et al.,eds.,Proc.ODP,initial results.184:college station,TX(ocean drilling program),1-77.doi:10.2973/odp.proc.ir.184.101.2000
Sibuet,J.C.,1992.New constraints on the formation of thenon-volcanic continental Galicia-Flemish Cap conjugatemargins.Journal of the Ceological Society,149(5):829-840.doi:10.1144/gsgs.149.5.0829
Sun,L.T.,Sun,Z.,Zhan,W.H.,et al.,2010.Petroleum potential prediction of the Lile basin in Nansha.Earth Science—Journal of China University of Geosciences,35(1):137-145(in Chinese with English abstract).
Sun,L.T.,Sun,Z.,Zhou,D.,et al.,2008.Stratigraphic andstructural characteristics of Lile basin in Nansha area.Geotectonica et Metallogenia,32(2):151-158(in Chinese with English abstract).
Sun,Z.,Zhong,Z.H.,Keep,M.,et al.,2009.3Danaloguemodeling of the South China Sea:a discussion onbreakup pattern.J.Asian.Earth.Sci.,34(4):544556.doi:10.1016/j.jseaes.2008.09.002
Taylor,B.,Hayes,D.E.,1983.Origin and history of theSouth China Sea basin.In:Hayes,D.E.,ed.,The tectonic and geologic evolution of the Southeast Asian seasand islands.Part2,Geophys.Monogr.,AGU,Washington,D.C.,23-56.
Whitmarsh,R.B.,Manatschal,G.,Minshull,T.A.,2001.Evolution of magma-poor continental margins from rifting to seafloor spreading.Nature,413:150-154.doi:10.1038/35093085
Williams,H.H.,1997.Play concepts—northwest Palawan,Philippines.J.Asian.Earth.Sci.,15(2-3):251273.doi:10.1016/S0743-9547(97)00011-1
Yan,P.,Liu,H.L.,2004.Tectonic-stratigraphic division andblind fold structures in Nansha waters,South ChinaSea.J.Asian.Earth.Sci.,24:337-348.
Yao,B.C.,Zeng,W.J.,Hayes,D.E.,1994.The geologicalmemoir of South China Sea surveyed by jointly China&U.S.A..China University of Geosciences Press,Wuhan(in Chinese).
Zhang,L.,Li,W.C.,Zeng,X.H.,2003.Stratigraphic sequence and hydrocarbon potential in Lile basin.Petroleum Geology&Experiment,25(5):469-480(in Chinese with English abstract).
Zhou,D.,Ru,K.,Chen,H.Z.,1995.Kinematics of Cenozoicextension on the South China Sea continental marginand its implications for the tectonic evolution of the region.Tectonophysics,251(1-4):161-177.doi:10.1016/0040.1951(95)00018-6
Ziegler,P.A.,1983.Crustal thinning and subsidence in theNorth Sea.Nature,304(5926):561.doi:10.1038/304561a0
高红芳,曾祥辉,刘振湖,等,2005.南海礼乐盆地沉降史模拟及构造演化特征分析.大地构造与成矿学,29(3):385-390.
李家彪,2008.中国边缘海形成演化与资源效应.北京:海洋出版社.
孙龙涛,孙珍,詹文欢,等,2010.南沙海域礼乐盆地油气资源潜力.地球科学——中国地质大学学报,35(1):137-145.
孙龙涛,孙珍,周蒂,等,2008.南沙海区礼乐盆地沉积地层与构造特征分析.大地构造与成矿学,32(2):151-158.
姚伯初,曾维军,Hayes,D.E.,1994.中美合作调研南海地质专报.武汉:中国地质大学出版社.
张莉,李文成,曾祥辉,2003.礼乐盆地地层发育特征及其与油气的关系.石油实验地质,25(5):469-480.
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