琼东南盆地构造沉降史及其主控因素
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摘要
以28口钻井、3条主干地震剖面最新解释成果资料为依据的构造沉降史恢复结果表明:琼东南盆地新生代存在三期快速沉降过程和一期缓慢沉降过程:第一期为始新世,第二期为渐新世—早中新世,第三期存在时空差异:在盆地西部乐东凹陷为晚中新世以来,在盆地中东部陵水凹陷和松南-宝岛凹陷为上新世以来;缓慢沉降过程亦存在时空差异,盆地西部中中新世沉降缓慢,盆地中东部中—晚中新世沉降缓慢.第一期快速沉降过程受东亚陆缘扩张和红河断裂左旋走滑共同影响,第二期快速沉降受南海海底扩张和红河断裂左旋走滑联合作用,第三期快速沉降主要受红河断裂右旋走滑控制,缓慢沉降过程与南海海底扩张停止以及红河断裂构造活动处于宁静阶段相耦合.
Based on the data from 28 boreholes and the latest data of 3 seismic lines, the estimation of tectonic subsidence shows that Qiongdongnan Basin (QDNB) experienced three episodes of rapid subsiding and one episode of weak subsiding in Cenozoic time. During Eocene and Oligocene to early Miocene time, both western and eastern QDNB underwent two episodes of rapid subsiding with different subsidence rates. There came a weak subsiding period from 16 Ma to 10.5 Ma in western QDNB and from 16 Ma to 5.3 Ma in mid-eastern QDNB. A rapid subsiding event occurred again at 10.5 Ma in the west and at 5.3 Ma in the mid-east areas of QDNB. The first rapid subsiding was a result of the combination of extension of Eastern Asia continental margin and the sinistral strike-slip of Red River Fault (RRF) in Eocene; the second one was related with the seafloor spreading of the South China Sea (SCS) and sinistral strike-slip of RRF in Oligocene to early Miocene; the third one is mainly controlled by the dextral strike-slip of RRF since 10～5 Ma; the weak subsiding process was coeval with the weakly strike-slipping period of RRF within mid-late Miocene time and a response to the cease of the seafloor spreading of SCS.
Based on the data from 28 boreholes and the latest data of 3 seismic lines, the estimation of tectonic subsidence shows that Qiongdongnan Basin (QDNB) experienced three episodes of rapid subsiding and one episode of weak subsiding in Cenozoic time. During Eocene and Oligocene to early Miocene time, both western and eastern QDNB underwent two episodes of rapid subsiding with different subsidence rates. There came a weak subsiding period from 16 Ma to 10.5 Ma in western QDNB and from 16 Ma to 5.3 Ma in mid-eastern QDNB. A rapid subsiding event occurred again at 10.5 Ma in the west and at 5.3 Ma in the mid-east areas of QDNB. The first rapid subsiding was a result of the combination of extension of Eastern Asia continental margin and the sinistral strike-slip of Red River Fault (RRF) in Eocene; the second one was related with the seafloor spreading of the South China Sea (SCS) and sinistral strike-slip of RRF in Oligocene to early Miocene; the third one is mainly controlled by the dextral strike-slip of RRF since 10～5 Ma; the weak subsiding process was coeval with the weakly strike-slipping period of RRF within mid-late Miocene time and a response to the cease of the seafloor spreading of SCS.
引文
[1]孙珍,钟志洪,周蒂等.红河断裂带的新生代变形机制及莺歌海盆地的实验证据.热带海洋学报,2003,22(2):1~9Sun Z,Zhong Z H,Zhou D,et al.Deformation mechanismof Red River Fault zone during Cenozoic and experimental evidences related to Yinggehai Basin formation.J.Tropical Oceanography(in Chinese),2003,22(2):1~9
[2]何廉声.南海的形成、演化与油气资源.海洋地质与第四纪地质,1988,8(2):15~28He L S.Origin and evolution of South China Sea and hydrocarbon resources.Marine Geology&Quaternary Geology(in Chinese),1988,8(2):15~28
[3]林长松,虞夏军,何拥华等.南海海盆扩张成因质疑.海洋学报,2006,28(1):67~76Lin C S,Yu XJ,He Y H,et al.Question onthe spreading of the South China Sea Basin.Acta Oceanological Sinica(in Chinese),2006,28(1):67~76
[4]刘绍文,施小斌,王良书等.南海成因机制及北部岩石圈热-流变结构研究进展.海洋地质与第四纪地质,2006,26(4):117~124Liu S W,Shi X B,Wang LS,et al.Recent advancesin studies on the formation mechanism of the South China Sea and thermo-rheological structure of lithosphere in its northern margin:an overview.Marine Geology&Quaternary Geology(in Chinese),2006,26(4):117~124
[5]郑勇,傅容珊,熊熊.中国大陆及周边地区现代岩石圈演化动力学模拟.地球物理学报,2006,49(2):415~427Zheng Y,Fu R S,Xiong X.Dynamic simulation of lithospheric evolutionfromthe modern China mainland andits surrounding areas.Chinese J.Geophys.(in Chinese),2006,49(2):415~427
[6]徐果明,姚华建,朱良保等.中国西部及其邻域地壳上地幔横波速度结构.地球物理学报,2007,50(1):193~208Xu G M,Yao HJ,Zhu L B,et a1.Shear wave velocitystructure of the crust and upper mantle in western China and its adjacent area.Chinese J.Geophys.(in Chinese),2007,50(1):193~208
[7]向宏发,万景林,韩竹军等.红河断裂带大型右旋走滑运动发生时代的地质分析与FT测年.中国科学(D辑),2006,36(11):977~987Xiang HF,Wan J L,Han Z J,et al.Geological analysis and FT dating of the large-scale right-lateral strike-slip movement of the Red Riverfault zone.Science in China(Ser.D Earth Sciences)(in Chinese),2006,36(11):977~987
[8]张进江,钟大赉,桑海清等.哀牢山—红河构造带古新世以来多期活动的构造和年代学证据.地质科学,2006,(2):291~310Zhang J J,Zhong D L,Sang H Q,et al.Structural and geochronological evidence for multiple episodes of deformation since Paleocene along the Ailao Shan-Red River shear zone,southeastern Asia.Chinese J.Geology(in Chinese),2006,(2):291~310
[9]龚再升,李思田,谢泰俊等.南海北部大陆边缘盆地分析与油气聚集.北京:科学出版社,1997Gong Z S,Li S T,Xie TJ,et al.Continental Margin Basin Analysis and Hydrocarbon Accumulation of the Northern South China Sea(in Chinese).Beijing:Science Press,1997
[10]龚再升.中国近海大油气田.北京:石油工业出版社,1997Gong Z S.The Major Oil and Gas Fields of China Offshore(in Chinese).Beijing:PetroleumIndustry Press,1997
[11]李绪宣,朱光辉.琼东南盆地断裂系统及其油气输导特征.中国海上油气,2005,17(1):1~7Li X X,Zhu G H.The fault system and its hydrocarbon carrier significance in Qiongdongnan basin.China Offshore Oil and Gas(in Chinese),2005,17(1):1~7
[12]于鹏,王家林,钟慧智等.琼东南盆地基底结构综合地球物理研究.中国海上油气(地质),1999,13(6):443~450Yu P,Wang J L,Zhong HZ,et al.Comprehensive geophysical research on the basement structure in Qiongdongnan Basin.China Offshore Oil and Gas(Geology)(in Chinese),1999,13(6):443~450
[13]张功成.中国近海天然气地质特征与勘探新领域.中国海上油气,2005,7(5):289~296Zhang GC.Geological features and newexplorationrealms of offshore gasin China.China Offshore Oil and Gas(in Chinese),2005,7(5):289~296
[14]李绪宣,钟志洪,董伟良等.琼东南盆地古近纪裂陷构造特征及其动力学机制.石油勘探与开发,2006,33(6):713~721Li X X,Zhong Z H,Dong WL,et al.Paleogene rift structure and its dynamics of Qiongdongnan Basin.Petroleum Exploration and Development(in Chinese),2006,33(6):713~721
[15]Springer J.Decompaction and backstripping with regard to erosion,salt movement,and interlayered bedding.Computers&Geosciences,1993,19(8):1115~1125
[16]陈国达.东亚陆缘扩张带——一条离散式大陆边缘成因的探讨.大地构造与成矿学,1997,21(4):285~293Chen G D.The marginal extensional belt of East Asia continental:investigatingthe origin of a discrete continental margin.Geotectonica et Metallogenia(in Chinese),1997,21(4):285~293
[17]张健,石耀霖.东亚陆缘带构造扩张的深部热力学机制.大地构造与成矿学,2003,27(3):222~227Zhang J,Shi Y L.Thermodynamics mechanism of the marginal extensional belt of East Asia.Geotectonica et Metallogenia(in Chinese),2003,27(3):222~227
[18]刘昭蜀,杨树康,何尚谋.南海陆缘地堑系及边缘海的演化旋回.热带海洋,1983,2(4):251~259Liu Z S,Yang S K,He S M.Grabensystemof continental margin of South China Sea and evolution cycles of marginal seas.Tropical Oceanology(in Chinese),1983,2(4):251~259
[19]孙肇才.从东海石油地质重要进展看西太平洋大陆边缘新生代盆地的构造演化——一种海沟向洋后退的残余弧后盆地演化模式.海相油气地质,2004,9(1-2):1~17Sun Z C.Progress of petroleumgeology research for the East China Sea and on tectonic evolution of Cenozoic basins in the continental margins along the West Pacific Ocean:an evolutional model of oceanwards-receding residual rear-arc basins.Marine Oil and Gas Geology(in Chinese),2004,9(1-2):1~17
[20]刘昭蜀,陈忠,潘宇.关于南海海盆的成因演化的探讨.见:李继亮编.中国东南海陆岩石圈结构与演化研究.北京:中国科学技术出版社,1992Liu Z S,Chen Z,Pan Y.Discussionof the originof South China Sea Basin.In:Li J L ed.Research of the Structure and Evolution of Oceanic and Continental Lithosphere of South China(in Chinese).Beijing:Chinese Science and Technology Press,1992
[21]朱炳泉,常向阳,胡跃国等.56Ma:华南岩石圈伸展和南海张开的重要转折时间.矿物岩石地球化学通报,2001,20(4):251~252Zhu B Q,Chang X Y,Hu Y G,et al.56Ma:An important transition age for extension of the Cathaysian lithosphere and open of the South China Sea.Bulletin of Mineralogy,Petrology and Geochemistry(in Chinese),2001,20(4):251~252
[22]Taylor B,Hayes DE.Thetectonic evolution of the South China Sea.In:Hayes D E ed.The Tectonic and Geological Evolution of Southeast Asia Seas and Islands.Geophys.Mono.Ser.,AGU,Washington D.C.,1980,23:89~104
[23]Ru K,Pigott J D.Episodic rifting and subsidence inthe South China Sea.AAPG Bulletin,1986,70(9):1136~1155
[24]Briais A,Patriat P,Tapponnier P,et al.Updated interpretation of magnetic anomalies and seafloor spreading stages in the South China Sea:implications for the Tertiary tectonics of Southeast Asia.J.Geophys.Res.,1993,98(B4):6299~6328
[25]姚伯初.南海海盆新生代的构造演化史.海洋地质与第四纪地质,1996,16(2):1~13Yao B C.Tectonic evolution of the South China Sea in Cenozoic.Marine Geology&Quaternary Geology(in Chinese),1996,16(2):1~13
[26]何廉声.南海地质构造图.何廉声主编.南海地质地球物理图集.广州:广东省地图出版社,1987He LS.Geological structure map of South China Sea.In:He L S ed.Geology and Geophysics Atlas of South China Sea(in Chinese).Guangzhou:Cartographic Publishing House of Guangdong Province,1987
[27]Taylor B,Hayes D E.Origin and history of the South China Sea basin.In:Hayes D E ed.The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands.Geophys.Mono.Ser.,AGU,Washington D.C.,1983,27:23~56
[28]Hayes D E,Spangle S,Zeng W,et al.Age and evolution of the South China Sea Southwest Sub-basin.EOS,Trans.Am.Geophys.Union,1987,68:14~96
[29]姚伯初.南海西北海盆的构造特征及南海新生代的海底扩张.热带海洋,1999,18(1):7~15Yao B C.Tectonic characteristics of northwest subbasin and seafloor spreading history of South China Sea in Cenozoic.Tropical Oceanology(in Chinese),1999,18(1):7~15
[30]刘昭蜀,陈雪.南海中央海盆热流值的分布特征及年代分析.地质科学,1987,(2):251~259Liu Z S,Chen X.Characteristics of heat flowdistributionin Central Basin of South China Sea and chronological implications.Chinese J.Geology(in Chinese),1987,(2):251~259
[31]袁玉松.南海北部陆缘深水区构造-热演化与烃源岩成熟度史[博士论文].北京:中国科学院地质与地球物理研究所,2007Yuan Y S.Tectonothermal evolution and source rock maturation historyin deep water area of the northern margin of the South China Sea[Ph.D.thesis](in Chinese).Beijing:Institute of Geology and Geophysics,Chinese Academy of Sciences,2007
[32]Hamilton W.Tectonics of the Indonesian region.US Geol.Survey Prof.Paper,1979,345~1078
[33]Holloway N H.North Palawan block,Philippines—Its relation to Asian mainland and role in evolution of South China Sea.Am.Assoc.Pet.Geol.Bull.,1982,66:1355~1383
[34]Fuller M,Mccabe R,WilliamsI S,et al.Paleomagnetismof Luzon.In:Hayes D E ed.The Tectonic and Geologic Evolution of Southeastern Asian Seas and Islands.Geophys.Mono.Ser.,AGU,Washington D.C.,1983,27:79~94
[35]徐震,徐鸣洁,王良书等.用接收函数Ps转换波研究地壳各向异性——以哀牢山—红河断裂带为例.地球物理学报,2006,49(2):438~448Xu Z,Xu MJ,Wang LS,et a1.Astudy on crustal anisotropy using P to S converted phase of the receiver function:application to Ailaoshan-Red Riverfault zone.Chinese J.Geophys.(in Chinese),2006,49(2):438~448
[36]Allen C R,Gillepsie AR,Han Y,et al.Red River and associated faults,Yunnan Province,China:Quaternary geology,slip rate,and seismic hazard.Geol.Soc.Amer.Bull.,1984,95:686~700
[37]Tapponnier P,Peltzer G,Armijo R,et al.Onthe mechanics of the collision between India and Asia.In:Coward MP,Ries A C eds.Collision Tectonics.Geol.Soc.Lond.Spec.Publ.,Blackwell Scientific,Oxford,1986,19:115~157
[38]钟大赉,Tapponnier P,吴海威.大型走滑断裂——碰撞后陆内变形的重要形式.科学通报,1989,34(7):525~529Zhong DL,Tapponnier P,Wu HW.Large scale strike-slipfault:a major pattern of intracontinenetal deformation after collision.Chinese Science Bulletin(in Chinese),1989,34(7):525~529
[39]陈文寄,Harrison T M,Lovera O M.哀牢山—红河剪切带的热年代学研究:多重扩散域模式的应用实例.地震地质,1992,4(2):121~128Chen WJ,Harrison T M,Lovera O M.Thermochronology of the Ailoshan-Red River shear zone:a case study of multiple diffusion domain model.Seismologyand Geology(in Chinese),1992,4(2):121~128
[40]Leloup P H,Lacassin R,Tapponnier P,et al.The Ailao Shan-Red River shear zone(Yunnan,China),Tertiary transformboundary of Indochina.Tectonophysics,1995,251:1~84
[41]万京林,李齐,陈文寄.哀牢山—红河左旋走滑剪切带构造抬升时间序列的裂变径迹证据.地震地质,1997,19(1):87~90Wan J L,Li Q,Chen WJ.Fission track evidence of diachronic uplift alongthe Ailao Shan-Red Riverleftlateral strike-slipshearzone.Seismology and Geology(in Chinese),1997,19(1):87~90
[42]Gilley L D,Harrison T M,Leloup P H,et al.Direct dating of left-lateral deformation along the Red River shear zone,China and Vietnam.J.Geophys.Res.,2003,10(B):Art.No.:2127
[43]向宏发,韩竹军,虢顺民等.红河断裂带大型右旋走滑运动定量研究的若干问题.地球科学进展,2004,19(增刊):56~59Xiang HF,Han ZJ,Guo S M,et al.Processing about quantitative study of large-scale strike-slip movement on Red River Fault zone.Advance in Earth Sciences(in Chinese),2004,19(Suppl.):56~59
[44]Tapponnier P,Lacassin R,Leloup P H,et al.The Ailao Shan-Red River metamorphic belt:Tertiaryleft-lateral shear between Indochina and South China.Nature,1990,343:431~437
[45]Chung S L,Lee T Y,Lo C H,et al.Intraplate extension prior to continental extrusion along the Ailao Shan-Red River shear zone.Geology,1997,25:311~314
[46]Wang J H,Yin A,Harrison T M,et al.A tectonic model for Cenozoic igneous activities in the eastern Indo-Asian collision zone.Earth Planet Sci.Lett.,2001,188:123~133
[47]Replumaz A,Lacassin R,Tapponnier P,et al.Large river oddsets and Pliocene-Quaternary dextral slip rate on the Red River fault(Yunnan,China).J.Geophys.Res.,2001,106(B1):819~836
[48]江为为,郝天珧,胥颐等.中国中南地区综合地质地球物理研究.地球物理学报,2007,50(1):171~183Jiang WW,Hao T Y,Xu Y,et al.Comprehensive geological and geophysical study in middle southern region of China.Chinese J.Geophy(in Chinese),2007,50(1):171~183
[49]孙珍,钟志洪,周蒂.莺歌海盆地构造演化与强烈沉降机制的分析和模拟.地球科学:中国地质大学学报,2007,32(3):347~356Sun Z,Zhong Z H,Zhou D.The analysis and analogue modeling of the tectonic evolution and strong subsidence in the Yinggehai Basin.Earth Science-Journal of China University of Geosciences(in Chinese),2007,32(3):347~356
[2]何廉声.南海的形成、演化与油气资源.海洋地质与第四纪地质,1988,8(2):15~28He L S.Origin and evolution of South China Sea and hydrocarbon resources.Marine Geology&Quaternary Geology(in Chinese),1988,8(2):15~28
[3]林长松,虞夏军,何拥华等.南海海盆扩张成因质疑.海洋学报,2006,28(1):67~76Lin C S,Yu XJ,He Y H,et al.Question onthe spreading of the South China Sea Basin.Acta Oceanological Sinica(in Chinese),2006,28(1):67~76
[4]刘绍文,施小斌,王良书等.南海成因机制及北部岩石圈热-流变结构研究进展.海洋地质与第四纪地质,2006,26(4):117~124Liu S W,Shi X B,Wang LS,et al.Recent advancesin studies on the formation mechanism of the South China Sea and thermo-rheological structure of lithosphere in its northern margin:an overview.Marine Geology&Quaternary Geology(in Chinese),2006,26(4):117~124
[5]郑勇,傅容珊,熊熊.中国大陆及周边地区现代岩石圈演化动力学模拟.地球物理学报,2006,49(2):415~427Zheng Y,Fu R S,Xiong X.Dynamic simulation of lithospheric evolutionfromthe modern China mainland andits surrounding areas.Chinese J.Geophys.(in Chinese),2006,49(2):415~427
[6]徐果明,姚华建,朱良保等.中国西部及其邻域地壳上地幔横波速度结构.地球物理学报,2007,50(1):193~208Xu G M,Yao HJ,Zhu L B,et a1.Shear wave velocitystructure of the crust and upper mantle in western China and its adjacent area.Chinese J.Geophys.(in Chinese),2007,50(1):193~208
[7]向宏发,万景林,韩竹军等.红河断裂带大型右旋走滑运动发生时代的地质分析与FT测年.中国科学(D辑),2006,36(11):977~987Xiang HF,Wan J L,Han Z J,et al.Geological analysis and FT dating of the large-scale right-lateral strike-slip movement of the Red Riverfault zone.Science in China(Ser.D Earth Sciences)(in Chinese),2006,36(11):977~987
[8]张进江,钟大赉,桑海清等.哀牢山—红河构造带古新世以来多期活动的构造和年代学证据.地质科学,2006,(2):291~310Zhang J J,Zhong D L,Sang H Q,et al.Structural and geochronological evidence for multiple episodes of deformation since Paleocene along the Ailao Shan-Red River shear zone,southeastern Asia.Chinese J.Geology(in Chinese),2006,(2):291~310
[9]龚再升,李思田,谢泰俊等.南海北部大陆边缘盆地分析与油气聚集.北京:科学出版社,1997Gong Z S,Li S T,Xie TJ,et al.Continental Margin Basin Analysis and Hydrocarbon Accumulation of the Northern South China Sea(in Chinese).Beijing:Science Press,1997
[10]龚再升.中国近海大油气田.北京:石油工业出版社,1997Gong Z S.The Major Oil and Gas Fields of China Offshore(in Chinese).Beijing:PetroleumIndustry Press,1997
[11]李绪宣,朱光辉.琼东南盆地断裂系统及其油气输导特征.中国海上油气,2005,17(1):1~7Li X X,Zhu G H.The fault system and its hydrocarbon carrier significance in Qiongdongnan basin.China Offshore Oil and Gas(in Chinese),2005,17(1):1~7
[12]于鹏,王家林,钟慧智等.琼东南盆地基底结构综合地球物理研究.中国海上油气(地质),1999,13(6):443~450Yu P,Wang J L,Zhong HZ,et al.Comprehensive geophysical research on the basement structure in Qiongdongnan Basin.China Offshore Oil and Gas(Geology)(in Chinese),1999,13(6):443~450
[13]张功成.中国近海天然气地质特征与勘探新领域.中国海上油气,2005,7(5):289~296Zhang GC.Geological features and newexplorationrealms of offshore gasin China.China Offshore Oil and Gas(in Chinese),2005,7(5):289~296
[14]李绪宣,钟志洪,董伟良等.琼东南盆地古近纪裂陷构造特征及其动力学机制.石油勘探与开发,2006,33(6):713~721Li X X,Zhong Z H,Dong WL,et al.Paleogene rift structure and its dynamics of Qiongdongnan Basin.Petroleum Exploration and Development(in Chinese),2006,33(6):713~721
[15]Springer J.Decompaction and backstripping with regard to erosion,salt movement,and interlayered bedding.Computers&Geosciences,1993,19(8):1115~1125
[16]陈国达.东亚陆缘扩张带——一条离散式大陆边缘成因的探讨.大地构造与成矿学,1997,21(4):285~293Chen G D.The marginal extensional belt of East Asia continental:investigatingthe origin of a discrete continental margin.Geotectonica et Metallogenia(in Chinese),1997,21(4):285~293
[17]张健,石耀霖.东亚陆缘带构造扩张的深部热力学机制.大地构造与成矿学,2003,27(3):222~227Zhang J,Shi Y L.Thermodynamics mechanism of the marginal extensional belt of East Asia.Geotectonica et Metallogenia(in Chinese),2003,27(3):222~227
[18]刘昭蜀,杨树康,何尚谋.南海陆缘地堑系及边缘海的演化旋回.热带海洋,1983,2(4):251~259Liu Z S,Yang S K,He S M.Grabensystemof continental margin of South China Sea and evolution cycles of marginal seas.Tropical Oceanology(in Chinese),1983,2(4):251~259
[19]孙肇才.从东海石油地质重要进展看西太平洋大陆边缘新生代盆地的构造演化——一种海沟向洋后退的残余弧后盆地演化模式.海相油气地质,2004,9(1-2):1~17Sun Z C.Progress of petroleumgeology research for the East China Sea and on tectonic evolution of Cenozoic basins in the continental margins along the West Pacific Ocean:an evolutional model of oceanwards-receding residual rear-arc basins.Marine Oil and Gas Geology(in Chinese),2004,9(1-2):1~17
[20]刘昭蜀,陈忠,潘宇.关于南海海盆的成因演化的探讨.见:李继亮编.中国东南海陆岩石圈结构与演化研究.北京:中国科学技术出版社,1992Liu Z S,Chen Z,Pan Y.Discussionof the originof South China Sea Basin.In:Li J L ed.Research of the Structure and Evolution of Oceanic and Continental Lithosphere of South China(in Chinese).Beijing:Chinese Science and Technology Press,1992
[21]朱炳泉,常向阳,胡跃国等.56Ma:华南岩石圈伸展和南海张开的重要转折时间.矿物岩石地球化学通报,2001,20(4):251~252Zhu B Q,Chang X Y,Hu Y G,et al.56Ma:An important transition age for extension of the Cathaysian lithosphere and open of the South China Sea.Bulletin of Mineralogy,Petrology and Geochemistry(in Chinese),2001,20(4):251~252
[22]Taylor B,Hayes DE.Thetectonic evolution of the South China Sea.In:Hayes D E ed.The Tectonic and Geological Evolution of Southeast Asia Seas and Islands.Geophys.Mono.Ser.,AGU,Washington D.C.,1980,23:89~104
[23]Ru K,Pigott J D.Episodic rifting and subsidence inthe South China Sea.AAPG Bulletin,1986,70(9):1136~1155
[24]Briais A,Patriat P,Tapponnier P,et al.Updated interpretation of magnetic anomalies and seafloor spreading stages in the South China Sea:implications for the Tertiary tectonics of Southeast Asia.J.Geophys.Res.,1993,98(B4):6299~6328
[25]姚伯初.南海海盆新生代的构造演化史.海洋地质与第四纪地质,1996,16(2):1~13Yao B C.Tectonic evolution of the South China Sea in Cenozoic.Marine Geology&Quaternary Geology(in Chinese),1996,16(2):1~13
[26]何廉声.南海地质构造图.何廉声主编.南海地质地球物理图集.广州:广东省地图出版社,1987He LS.Geological structure map of South China Sea.In:He L S ed.Geology and Geophysics Atlas of South China Sea(in Chinese).Guangzhou:Cartographic Publishing House of Guangdong Province,1987
[27]Taylor B,Hayes D E.Origin and history of the South China Sea basin.In:Hayes D E ed.The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands.Geophys.Mono.Ser.,AGU,Washington D.C.,1983,27:23~56
[28]Hayes D E,Spangle S,Zeng W,et al.Age and evolution of the South China Sea Southwest Sub-basin.EOS,Trans.Am.Geophys.Union,1987,68:14~96
[29]姚伯初.南海西北海盆的构造特征及南海新生代的海底扩张.热带海洋,1999,18(1):7~15Yao B C.Tectonic characteristics of northwest subbasin and seafloor spreading history of South China Sea in Cenozoic.Tropical Oceanology(in Chinese),1999,18(1):7~15
[30]刘昭蜀,陈雪.南海中央海盆热流值的分布特征及年代分析.地质科学,1987,(2):251~259Liu Z S,Chen X.Characteristics of heat flowdistributionin Central Basin of South China Sea and chronological implications.Chinese J.Geology(in Chinese),1987,(2):251~259
[31]袁玉松.南海北部陆缘深水区构造-热演化与烃源岩成熟度史[博士论文].北京:中国科学院地质与地球物理研究所,2007Yuan Y S.Tectonothermal evolution and source rock maturation historyin deep water area of the northern margin of the South China Sea[Ph.D.thesis](in Chinese).Beijing:Institute of Geology and Geophysics,Chinese Academy of Sciences,2007
[32]Hamilton W.Tectonics of the Indonesian region.US Geol.Survey Prof.Paper,1979,345~1078
[33]Holloway N H.North Palawan block,Philippines—Its relation to Asian mainland and role in evolution of South China Sea.Am.Assoc.Pet.Geol.Bull.,1982,66:1355~1383
[34]Fuller M,Mccabe R,WilliamsI S,et al.Paleomagnetismof Luzon.In:Hayes D E ed.The Tectonic and Geologic Evolution of Southeastern Asian Seas and Islands.Geophys.Mono.Ser.,AGU,Washington D.C.,1983,27:79~94
[35]徐震,徐鸣洁,王良书等.用接收函数Ps转换波研究地壳各向异性——以哀牢山—红河断裂带为例.地球物理学报,2006,49(2):438~448Xu Z,Xu MJ,Wang LS,et a1.Astudy on crustal anisotropy using P to S converted phase of the receiver function:application to Ailaoshan-Red Riverfault zone.Chinese J.Geophys.(in Chinese),2006,49(2):438~448
[36]Allen C R,Gillepsie AR,Han Y,et al.Red River and associated faults,Yunnan Province,China:Quaternary geology,slip rate,and seismic hazard.Geol.Soc.Amer.Bull.,1984,95:686~700
[37]Tapponnier P,Peltzer G,Armijo R,et al.Onthe mechanics of the collision between India and Asia.In:Coward MP,Ries A C eds.Collision Tectonics.Geol.Soc.Lond.Spec.Publ.,Blackwell Scientific,Oxford,1986,19:115~157
[38]钟大赉,Tapponnier P,吴海威.大型走滑断裂——碰撞后陆内变形的重要形式.科学通报,1989,34(7):525~529Zhong DL,Tapponnier P,Wu HW.Large scale strike-slipfault:a major pattern of intracontinenetal deformation after collision.Chinese Science Bulletin(in Chinese),1989,34(7):525~529
[39]陈文寄,Harrison T M,Lovera O M.哀牢山—红河剪切带的热年代学研究:多重扩散域模式的应用实例.地震地质,1992,4(2):121~128Chen WJ,Harrison T M,Lovera O M.Thermochronology of the Ailoshan-Red River shear zone:a case study of multiple diffusion domain model.Seismologyand Geology(in Chinese),1992,4(2):121~128
[40]Leloup P H,Lacassin R,Tapponnier P,et al.The Ailao Shan-Red River shear zone(Yunnan,China),Tertiary transformboundary of Indochina.Tectonophysics,1995,251:1~84
[41]万京林,李齐,陈文寄.哀牢山—红河左旋走滑剪切带构造抬升时间序列的裂变径迹证据.地震地质,1997,19(1):87~90Wan J L,Li Q,Chen WJ.Fission track evidence of diachronic uplift alongthe Ailao Shan-Red Riverleftlateral strike-slipshearzone.Seismology and Geology(in Chinese),1997,19(1):87~90
[42]Gilley L D,Harrison T M,Leloup P H,et al.Direct dating of left-lateral deformation along the Red River shear zone,China and Vietnam.J.Geophys.Res.,2003,10(B):Art.No.:2127
[43]向宏发,韩竹军,虢顺民等.红河断裂带大型右旋走滑运动定量研究的若干问题.地球科学进展,2004,19(增刊):56~59Xiang HF,Han ZJ,Guo S M,et al.Processing about quantitative study of large-scale strike-slip movement on Red River Fault zone.Advance in Earth Sciences(in Chinese),2004,19(Suppl.):56~59
[44]Tapponnier P,Lacassin R,Leloup P H,et al.The Ailao Shan-Red River metamorphic belt:Tertiaryleft-lateral shear between Indochina and South China.Nature,1990,343:431~437
[45]Chung S L,Lee T Y,Lo C H,et al.Intraplate extension prior to continental extrusion along the Ailao Shan-Red River shear zone.Geology,1997,25:311~314
[46]Wang J H,Yin A,Harrison T M,et al.A tectonic model for Cenozoic igneous activities in the eastern Indo-Asian collision zone.Earth Planet Sci.Lett.,2001,188:123~133
[47]Replumaz A,Lacassin R,Tapponnier P,et al.Large river oddsets and Pliocene-Quaternary dextral slip rate on the Red River fault(Yunnan,China).J.Geophys.Res.,2001,106(B1):819~836
[48]江为为,郝天珧,胥颐等.中国中南地区综合地质地球物理研究.地球物理学报,2007,50(1):171~183Jiang WW,Hao T Y,Xu Y,et al.Comprehensive geological and geophysical study in middle southern region of China.Chinese J.Geophy(in Chinese),2007,50(1):171~183
[49]孙珍,钟志洪,周蒂.莺歌海盆地构造演化与强烈沉降机制的分析和模拟.地球科学:中国地质大学学报,2007,32(3):347~356Sun Z,Zhong Z H,Zhou D.The analysis and analogue modeling of the tectonic evolution and strong subsidence in the Yinggehai Basin.Earth Science-Journal of China University of Geosciences(in Chinese),2007,32(3):347~356
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