摘要
青藏高原和南海分别是地球上最高的高原、东亚大陆边缘最大的边缘海,是地理位置紧邻的两个特殊地质单元。纵观青藏高原的隆升、挤出与南海的动力演化过程,二者存在一定的关联耦合性,而红河断裂带作为二者之间的纽带,直接控制了南海西北部陆缘岩石圈裂解及盆地的构造迁移和演化过程,并制约了盆地沉积地层充填和烃源岩的形成、分布,使得青藏高原与南海西北部盆地构成最为显著的盆-山耦合体系。由于区域动力背景的多层次性、多因素性及多变性,对于南海多期次多轴向复杂的构造特征及南海西北部陆缘新生代盆地构造沉积过程,与高原隆升、块体挤出的时空关系,至今无法给出完美的解释。综合前人研究成果,本文试图理清青藏隆升、挤出与南海形成演化过程的关系,总结现阶段研究中面临的诸多问题,在此基础上对未来的研究方向做出展望,以期促进对青藏隆升、块体挤出与南海盆地演化三者关系的合理理解。
As the adjacent geological units,the Tibetan Plateau and the SCS is respectively the highest plateau in the world and the largest continental marginal sea along the East Asian continental margin,showing their own characteristics and particularity.There is a certain coupling between the uplifting and extrusion of the Tibetan Plateau and the tectonic dynamic evolution of the SCS.Serving as a link between the Tibetan Plateau and the SCS,the Red River Fault Zone controlled the rupturing of continental lithosphere in the northwestern margin of the SCS and the tectonic migration and evolution of the northwestern SCS basins.Meanwhile,the sediments filling and the formation and distribution of hydrocarbon source rocks are even constrained by the fault zone,making the Tibetan Plateau-northwestern SCS basins being the most significant basin-mountain coupling system.However,owning to the characteristics of the multi-level,multi-factors,and variability of the regional dynamics,the relationship between the multi-stage and multi-axial evolution of the SCS and the tectono-sedimentary history of the northwestern SCS basins,and the uplifting and extrusion of the Tibetan Plateau are still open to intense debate.Based on the existing research achievements,this article tries to figure out the relationship between uplifting and extrusion of the Tibetan Plateau and tectonic dynamic evolution of the SCS.Additionally,the directions for future research have been anticipated in order to bring the clear understanding of the relationship among the three special geological units.
引文
[1]许志琴,王勤,李忠海,等.印度-亚洲碰撞:从挤压到走滑的构造转换[J].地质学报,2016,90(1):1-23.
[2]COPLEY A,AVOUAC J,ROYER J.India-Asia collision and the Cenozoic slowdown of the Indian plate:implications for the forces driving plate motions[J].Journal of Geophysical Research,2010,115:B03410.
[3]ROYDEN L H,BURCHFIEL B C,VAN DER HILST R D.The geological evolution of the Tibetan Plateau[J].Science,2008,321(5892):1054-1058.
[4]HALL R.Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific:computer-based reconstructions,model and animations[J].Journal of Asian Earth Sciences,2002,20(4):353-431.
[5]TAPPONNIER P,PELTZER G,LE DAIN A Y,et al.Propagating extrusion tectonics in Asia:new insights from simple experiments with plasticine[J].Geology,1982,10(12):611-616.
[6]郭令智,施央申,马瑞士.西太平洋中、新生代活动大陆边缘和岛弧构造的形成及演化[J].地质学报,1983(1):11-21.
[7]HONZA E.Spreading mode of backarc basins in the western Pacific[J].Tectonophysics,1995,251(1/2/3/4):139-152.
[8]MORLEY C K.A tectonic model for the Tertiary evolution of strike-slip faults and rift basins in SE Asia[J].Tectonophysics,2002,347(4):189-215.
[9]MORLEY C K.Late Cretaceous-Early Palaeogene tectonic development of SE Asia[J].Earth-Science Reviews,2012,115(1/2):37-75.
[10]HALL R,VAN HATTUM M W A,SPAKMAN W.Impact of India-Asia collision on SE Asia:the record in Borneo[J].Tectonophysics,2008,451(1/2/3/4):366-389.
[11]HALL R.Late Jurassic-Cenozoic reconstructions of the Indonesian region and the Indian Ocean[J].Tectonophysics,2012,570/571:1-41.
[12]XU J,BEN-AVRAHAM Z,KELTY T,et al.Origin of marginal basins of the NW Pacific and their plate tectonic reconstructions[J].Earth-Science Reviews,2014,130:154-196.
[13]TAPPONNIER P.Oblique stepwise rise and growth of the Tibet Plateau[J].Science,2001,294(5547):1671-1677.
[14]许志琴,李海兵,唐哲民,等.大型走滑断裂对青藏高原地体构架的改造[J].岩石学报,2011,27(11):3157-3170.
[15]RANGIN C,KLEIN M,ROQUES D,et al.The Red River fault system in the Tonkin Gulf,Vietnam[J].Tectonophysics,1995,243(3/4):209-222.
[16]CLIFT P,LEE G H,ANH DUC N,et al.Seismic reflection evidence for a dangerous grounds miniplate:no extrusion origin for the South China Sea[J].Tectonics,2008,27:TC3008.
[17]TAPPONNIER P,PELTZER G,ARMIJO R.On the mechanics of the collision between India and Asia[J].GeologicalSociety of London,Special Publication,1986,19(1):113-157.
[18]BRIAIS A,PATTIAT P,TAPPONNIER A P.Updated interpretation of magnetic anomalies and seafloor spreading stages in the South China Sea:implications for the Tertiary tectonics of southeast Asia[J].Journal of Geophysical Research,1993,98(B4):6299-6328.
[19]LELOUP P H,LACASSIN R,TAPPONNIER P,et al.The Ailao Shan-Red River shear zone(Yunnan,China),Tertiary transform boundary of Indochina[J].Tectonophysics,1995,251:3-84.
[20]LELOUP P H,ARNAUD N,LACASSIN R,et al.New constraints on the structure,thermochronology,and timing of the Ailao Shan-Red River shear zone,SE Asia[J].Journal of Geophysical Research,2001,106(B4):6683-6732.
[21]谢建华.南海新生代构造演化及其成因数值模拟[D].广州:中国科学院广州地球化学研究所,2006:55-72.
[22]MAZUR S,GREEN C,STEWART M G,et al.Displacement along the Red River Fault constrained by extension estimates and plate reconstructions[J].Tectonics,2012,31:TC5008.
[23]HUI G,LI S,GUO L,et al.Source and accumulation of gas hydrate in the northern margin of the South China Sea[J].Marine and Petroleum Geology,2016,69:127-145.
[24]MORLEY C K.Major unconformities/termination of extension events and associated surfaces in the South China Seas:review and implications for tectonic development[J].Journal of Asian Earth Sciences,2016,120:62-86.
[25]雷超,任建业,裴健翔,等.琼东南盆地深水区构造格局和幕式演化过程[J].地球科学:中国地质大学学报,2011,36(1):151-162.
[26]孙桂华,彭学超,黄永健.红河断裂带莺歌海段地质构造特征[J].地质学报,2013,87(2):154-166.
[27]钟志洪,王良书,夏斌,等.莺歌海盆地成因及其大地构造意义[J].地质学报,2004,78(3):302-309.
[28]NORTHRUP C J,ROYDEN L H,BURCHFIEL B C.Motion of the Pacific plate relative to Eurasia and its potential relation to Cenozoic extension along the eastern margin of Eurasia[J].Geology,1995,23(8):719-722.
[29]李武显,周新民.中国东南部晚中生代俯冲带探索[J].高校地质学报,1999,5(2):45-50.
[30]LI Z,LI X,CHUNG S,et al.Magmatic switch-on and switch-off along the South China continental margin since the Permian:transition from an Andean-type to a Western Pacific-type plate boundary[J].Tectonophysics,2012,532-535:271-290.
[31]LI Z,LI X.Formation of the 1300-km-wide intracontinental orogen and postorogenic magmatic province in Mesozoic South China:a flat-slab subduction model[J].Geology,2007,35(2):179.
[32]李三忠,索艳慧,刘鑫,等.南海的盆地群与盆地动力学[J].海洋地质与第四纪地质,2012,32(6):55-78.
[33]LIU J,TANG Y,TRAN M,et al.The nature of the Ailao Shan-Red River(ASRR)shear zone:constraints from structural,microstructural and fabric analyses of metamorphic rocks from the Diancang Shan,Ailao Shan and Day Nui Con Voi massifs[J].Journal of Asian Earth Sciences,2012,47:231-251.
[34]REN J,TAMAKI K,LI S,et al.Late Mesozoic and Cenozoic rifting and its dynamic setting in Eastern China and adjacent areas[J].Tectonophysics,2002,344(3/4):175-205.
[35]LEE T Y,LAWVER L A.Cenozoic plate reconstruction of southeast Asia[J].Tectonophysics,1995,251:85-138.
[36]孙珍,钟志洪,周蒂,等.南海的发育机制研究:相似模拟证据[J].中国科学:地球科学,2006,36(9):797-810.
[37]张亮.南海构造演化模式及其数值模拟[D].青岛:中国科学院海洋研究所,2012:122-123.
[38]周蒂,吴世敏,陈汉宗.南沙海区及邻区构造演化动力学的若干问题[J].大地构造与成矿学,2005,29(3):339-345.
[39]程世秀,李三忠,索艳慧,等.南海北部新生代盆地群构造特征及其成因[J].海洋地质与第四纪地质,2012,32(6):79-93.
[40]葛肖虹,王敏沛,刘俊来.重新厘定“四川运动”与青藏高原初始隆升的时代、背景:黄陵背斜构造形成的启示[J].地学前缘,2010,17(4):206-217.
[41]钟大赉,丁林.青藏高原的隆起过程及其机制探讨[J].中国科学:地球科学,1996,26(4):289-295.
[42]葛肖虹,任收麦,马立祥,等.青藏高原多期次隆升的环境效应[J].地学前缘,2006,13(6):118-130.
[43]张克信,王国灿,洪汉烈,等.青藏高原新生代隆升研究现状[J].地质通报,2013,32(1):1-18.
[44]XU Z Q,WANG Q,CAI Z H,et al.Kinematics of the Tengchong Terrane in SE Tibet from the late Eocene toearly Miocene:insights from coeval mid-crustal detachments andstrike-slip shear zones[J].Tectonophysics,2015,665:127-148.
[45]雷超,任建业,张静.南海构造变形分区及成盆过程[J].地球科学:中国地质大学学报,2015,40(4):744-762.
[46]雷超.南海北部莺歌海-琼东南盆地新生代构造变形格局及其演化过程分析[D].武汉:中国地质大学(武汉),2012:54-56,107.
[47]DOUST H,SUMNER H S.Petroleum systems in rift basins:a collective approach in Southeast Asian basins[J].Petroleum Geosciences,2007,13(2):127-144.
[48]TAPPONNIER P,LACASSIN R,LELOUP P H,et al.The Ailao Shan/Red River metamorphic belt:Tertiary left-lateral shear between Indochina and South China[J].Nature,1990,343:431-437.
[49]HARRISON T M,LELOUP P H,RYERSON F J,et al.Diachronous initiation of transtension along the Ailao ShanRed River shear zone,Yunnan and Vietnam[M]∥YIN A,HARRISON T M.Tectonic evolution of Asia.New York:Cambridge University Press,1996:208-226.
[50]张培震,张会平,郑文俊,等.东亚大陆新生代构造演化[J].地震地质,2014,36(3):574-585.
[51]SATO K,LIU Y,ZHU Z,et al.Tertiary paleomagnetic data from northwestern Yunnan,China:further evidence for large clockwise rotation of the Indochina block and its tectonic implications[J].Earth and Planetary Science Letters,2001,185(1/2):185-198.
[52]刘俊来,曹淑云,翟云峰,等.用陆块旋转解释藏东南渐新世—中新世伸展作用:来自点苍山及邻区变质核杂岩的证据[J].地学前缘,2007,14(4):40-48.
[53]OTOFUJI Y,TUNG V D,FUJIHARA M,et al.Tectonic deformation of the southeastern tip of the Indochina Peninsula during its southward displacement in the Cenozoic time[J].Gondwana Research,2012,22(2):615-627.
[54]TSUCHIYAMA Y,ZAMAN H,SOTHAM S,et al.Paleomagnetism of Late Jurassic to Early Cretaceous red beds from the Cardamom Mountains,southwestern Cambodia:tectonic deformation of the Indochina Peninsula[J].Earth and Planetary Science Letters,2016,434:274-288.
[55]郭令智,钟志洪,王良书,等.莺歌海盆地周边区域构造演化[J].高校地质学报,2001,7(1):1-12.
[56]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[J].热带海洋学报,2003,22(2):1-9.
[57]李家彪.南海大陆边缘动力学:科学实验与研究进展[J].地球物理学报,2011,54(12):2993-3003.
[58]HSU S,YEH Y,DOO W,et al.New bathymetry and magnetic lineations identifications in the northernmost South China Sea and their tectonic implications[J].Marine Geophysical Researches,2004,25(1/2):29-44.
[59]CULLEN A,REEMST P,HENSTRA G,et al.Rifting of the South China Sea:new perspectives[J].Petroleum Geoscience,2010,16(3):273-282.
[60]SIBUET J,YEH Y,LEE C.Geodynamics of the South China Sea[J].Tectonophysics,2016,692:98-119.
[61]FULLER M,ALI J R,MOSS S J,et al.Paleomagnetism of Borneo[J].Journal of Asian Earth Sciences,1999,17(1):3-24.
[62]LEVELL K B.The nature and significance of regional unconformities in the hydrocarbon-bearing Neogene sequence offshore West Sabah[J].Geological Society of Malaysia Bulletin,1987,21:55-90.
[63]HALL R.Contraction and extension in northern Borneo driven by subduction rollback[J].Journal of Asian Earth Sciences,2013,76:399-411.
[64]JIANG X,LI Z.Seismic reflection data support episodic and simultaneous growth of the Tibetan Plateau since 25Myr[J].Nature Communications,2014,5:5453.
[65]WANG E,KIRBY E,FURLONG K P,et al.Two-phase growth of high topography in eastern Tibet during the Cenozoic[J].Nature Geoscience,2012,5(9):640-645.
[66]CAO S,NEUBAUER F,LIU J,et al.Exhumation of the Diancang Shan metamorphic complex along the Ailao ShanRed River belt,southwestern Yunnan,China:evidence from40Ar/39Ar thermochronology[J].Journal of Asian Earth Sciences,2011,42(3):525-550.
[67]何家雄,张伟,颜文,等.中国近海盆地幕式构造演化及成盆类型与油气富集规律[J].海洋地质与第四纪地质,2014,34(2):121-134.
[68]REPLUMAZ A,TAPPONNIER P.Reconstruction of the deformed collision zone between India and Asia by backward motion of lithospheric blocks[J].Journal of Geophysical Research,2003,108(B6):2285.
[69]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].Journal of Geophysical Research,2003,108(B2):2127.
[70]LIU M,CUI X,LIU F.Cenozoic rifting and volcanism in eastern China:a mantle dynamic link to the Indo-Asian collision?[J].Tectonophysics,2004,393:29-42.
[71]陈文,张彦,张岳桥,等.青藏高原东南缘晚新生代幕式抬升作用的Ar-Ar热年代学证据[J].岩石学报,2006,22(4):867-872.
[72]张克信,王国灿,曹凯,等.青藏高原新生代主要隆升事件:沉积响应与热年代学记录[J].中国科学:地球科学,2008,38(12):1575-1588.
[73]THIEDE R C,ARROWSMITH J R,BOOKHAGEN B,et al.Dome formation and extension in the Tethyan Himalaya,Leo Pargil,northwest India[J].Geological Society of America Bulletin,2006,118(5/6):635-650.
[74]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[J].地质科学,2006,41(2):291-310.
[75]HINTERSBERGER E,THIEDE R C,STRECKER M R,et al.East-west extension in the NW Indian Himalaya[J].Geological Society of America Bulletin,2010,122(9/10):1499-1515.
[76]MITSUISHI M,WALLIS S R,AOYA M,et al.E-W extension at 19Ma in the Kung Co area,S.Tibet:evidence for contemporaneous E-W and N-S extension in the Himalayan orogen[J].Earth and Planetary Science Letters,2012,325/326:10-20.
[77]WANG E Q,BURCHFIEL B C,ROYDEN L H,et al.Late Cenozoic Xianshuihe-Xiaojiang,Red River,and Dali faultsystems of southwestern Sichuan and central Yunnan,China[J].Geological Society of America,Special Paper,1998,327:1-108.
[78]WANG E,BURCHFIEL B C.Late Cenozoic to Holocene deformation in southwestern Sichuan and adjacent Yunnan,China,and its role in formation of the southeastern part of the Tibetan Plateau[J].Geological Society of America Bulletin,2000,112(3):413-423.
[79]WANG Q,ZHANG P Z,FREYMUELLER J T,et al.Present-day crustal deformation in China constrained by global positioning system measurements[J].Science,2001,294:574-577.
[80]GAN W,ZHANG P,SHEN Z,et al.Present-day crustal motion within the Tibetan Plateau inferred from GPS measurements[J].Journal of Geophysical Research,2007,112:B08416.
[81]WANG S,FANG X,ZHENG D,et al.Initiation of slip along the Xianshuihe fault zone,eastern Tibet,constrained by K/Ar and fission-track ages[J].International Geology Review,2009,51(12):1121-1131.
[82]张远泽.川滇地块东部主要活动断裂新生代精确构造年代格架及其对青藏高原东缘新生代动力学过程的启示[D].武汉:中国地质大学(武汉),2015:75-80.
[83]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[J].中国科学:地球科学,2006,36(11):977-987.
[84]王二七,樊春,王刚,等.滇西哀牢山—点苍山形成的构造和地貌过程[J].第四纪研究,2006,26(2):220-227.
[85]王大伟,吴时国,李春峰,等.晚中新世红河断裂走滑反转事件的海底滑坡证据[J].中国科学:地球科学,2016,46(10):1349-1357.
[86]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.
[87]YAN P,WANG Y,LIU H.Post-spreading transpressive faults in the South China Sea Basin[J].Tectonophysics,2008,450:70-78.
[88]解习农,任建业,王振峰,等.南海大陆边缘盆地构造演化差异性及其与南海扩张耦合关系[J].地学前缘,2015,22(1):77-87.
[89]刘俊来,唐渊,宋志杰,等.滇西哀牢山构造带:结构与演化[J].吉林大学学报(地球科学版),2011,41(5):1285-1303.
[90]SEARLE M P,YEH M W,LIN T H,et al.Structural constraints on the timing of left-lateral shear along the Red River shear zone in the Ailao Shan and Diancang Shan Ranges,Yunnan,SW China[J].Geosphere,2010,6(4):316-338.
[91]刘海龄,姚永坚,沈宝云,等.南海西缘结合带的贯通性[J].地球科学:中国地质大学学报,2015,40(4):615-632.
[92]ANCZKIEWICZ R,VIOLA G,MüNTENER O,et al.Structure and shearing conditions in the Day Nui Con Voi massif:implications for the evolution of the Red River shear zone in northern Vietnam[J].Tectonics,2007,26:TC2002.
[93]李宝龙,季建清,付孝悦,等.滇西点苍山—哀牢山变质岩系变质时限研究[J].岩石学报,2009,25(3):595-608.
[94]白志明,王椿镛.云南遮放—宾川和孟连—马龙宽角地震剖面的层析成像研究[J].地球物理学报,2004,47(2):257-267.
[95]张恩会,楼海,嘉世旭,等.云南西部地壳深部结构特征[J].地球物理学报,2013,56(6):1915-1927.
[96]王夫运,潘素珍,刘兰,等.玉溪—临沧剖面宽角地震探测:红河断裂带及滇南地壳结构研究[J].地球物理学报,2014,57(10):3247-3258.
[97]BURCHFIEL B C,WANG E.Northwest-trending,middle Cenozoic,left-lateral faults in southern Yunnan,China,and their tectonic significance[J].Journal of Structural Geology,2003,25(5):781-792.
[98]SCHOENBOHM L M,BURCHFIEL B C,LIANGZHONG C,et al.Miocene to present activity along the Red River fault,China,in the context of continental extrusion,uppercrustal rotation,and lower-crustal flow[J].Geological Society of America Bulletin,2006,118(5/6):672-688.
[99]李宝龙,季建清,王丹丹,等.滇南新元古代的岩浆作用:来自瑶山群深变质岩SHRIMP锆石U-Pb年代学证据[J].地质学报,2012,86(10):1584-1591.
[100]王国灿,曹凯,张克信,等.青藏高原新生代构造隆升阶段的时空格局[J].中国科学:地球科学,2011,41(3):332-349.
[101]张连生,钟大赉.从红河剪切带走滑运动看东亚大陆新生代构造[J].地质科学,1996,31(4):327-341.
[102]CAO S,LIU J,LEISS B,et al.Oligo-Miocene shearing along the Ailao Shan-Red River shear zone:constraints from structural analysis and zircon U/Pb geochronology of magmatic rocks in the Diancang Shan massif,SE Tibet,China[J].Gondwana Research,2011,19(4):975-993.
[103]LU Y,KERRICH R,CAWOOD P A,et al.Zircon SHRIMP U-Pb geochronology of potassic felsic intrusions in western Yunnan,SW China:constraints on the relationship of magmatism to the Jinsha suture[J].Gondwana Research,2012,22(2):737-747.
[104]WANG P L,LO C H,LEE T Y,et al.Thermochronological evidence for the movement of the Ailao Shan-Red River shear zone:aperspective from Vietnam[J].Geology,1998,26(10):887-890.
[105]TANG Y,LIU J,TRAN M,et al.Timing of left-lateral shearing along the Ailao Shan-Red River shear zone:constraints from zircon U-Pb ages from granitic rocks in the shear zone along the Ailao Shan Range,Western Yunnan,China[J].International Journal of Earth Sciences,2013,102(3):605-626.
[106]宫伟,姜效典.哀牢山—红河断裂带哀牢山—大象山段渐新世—早中新世热史演化及成因[J].地球科学:中国地质大学学报,2017,42(2):223-239.
[107]CHEN X,LIU J,TANG Y,et al.Contrasting exhumation histories along a crustal-scale strike-slip fault zone:the Eocene to Miocene Ailao Shan-Red River shear zone in southeastern Tibet[J].Journal of Asian Earth Sciences,2015,114:174-187.
[108]CHUNG S L,LEE T Y,LO C H,et al.Intraplate extension prior to continental extrusion along the Ailao ShanRed River shear zone[J].Geology,1997,25(4):311-314.
[109]FYHN M B W,BOLDREEL L O,NIELSEN L H.Geological development of the Central and South Vietnamese margin:implications for the establishment of the South China Sea,Indochinese escape tectonics and Cenozoic volcanism[J].Tectonophysics,2009,478(3/4):184-214.
[110]万玲,吴能友.红河断裂带在南海海域的延伸[R].北京:中国地球物理学会,2001.
[111]刘宝明,夏斌,李绪宣,等.红河断裂带东南的延伸及其构造演化意义[J].中国科学:地球科学,2006,36(10):914-924.
[112]詹文欢,丘学林,孙宗勋,等.红河活动断裂带在南海西北部的反映[J].热带海洋学报,2003,22(2):10-16.
[113]ZHU M,GRAHAM S,MCHARGUE T.The Red River Fault zone in the Yinggehai Basin,South China Sea[J].Tectonophysics,2009,476(3/4):397-417.
[114]孙珍,周蒂,钟志洪,等.莺-琼盆地基底控制断裂样式的模拟探讨[J].热带海洋学报,2005,24(2):70-78.
[115]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[J].地球科学:中国地质大学学报,2007,32(3):347-356.
[116]朱伟林,张功成,高乐.南海北部大陆边缘盆地油气地质特征与勘探方向[J].石油学报,2008,29(1):1-9.
[117]朱伟林,吴景富,张功成,等.中国近海新生代盆地构造差异性演化及油气勘探方向[J].地学前缘,2015,22(1):88-101.
[118]颜丹平,周美夫,王焰,等.都龙-Song Chay变质穹隆体变形与构造年代:南海盆地北缘早期扩张作用始于华南地块张裂的证据[J].地球科学:中国地质大学学报,2005,30(4):402-412.
[119]任建业,庞雄,雷超,等.被动陆缘洋陆转换带和岩石圈伸展破裂过程分析及其对南海陆缘深水盆地研究的启示[J].地学前缘,2015,22(1):102-114.
[120]钟志洪,王良书,夏斌,等.莺歌海盆地成因及其大地构造意义[J].地质学报,2004,78(3):302-309.
[121]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[J].地震地质,1997,19(1):88-91.
[122]张进江,钟大赉,季建清,等.东喜马拉雅构造结大陆碰撞以来构造年代学框架及其与哀牢山红河构造带的对比[J].矿物岩石地球化学通报,2001,20(4):243-244.
[123]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[J].地球科学进展,2004,19(增刊1):56-59.
[124]WANG Y,ZHANG B,SCHOENBOHM L M,et al.Late Cenozoic tectonic evolution of the Ailao Shan-Red River fault(SE Tibet):implications for kinematic change during plateau growth[J].Tectonics,2016,35(8):1969-1988.
[125]向宏发,虢顺民,张晚霞,等.红河断裂带南段中新世以来大型右旋位错量的定量研究[J].地震地质,2007,29(1):34-50.
[126]SCHOENBOHM L M,WHIPPLE K X,BURCHFIEL B C,et al.Geomorphic constraints on surface uplift,exhumation,and plateau growth in the Red River region,Yunnan Province,China[J].Geological Society of America Bulletin,2004,116(7):895.
[127]李朝阳,姜效典,李德勇,等.红河断裂带中南段上新世以来构造隆升及成因[J].中国海洋大学学报(自然科学版),2016,46(7):90-98.
[128]袁玉松,杨树春,胡圣标,等.琼东南盆地构造沉降史及其主控因素[J].地球物理学报,2008,51(2):376-383.
[129]龚再升,李思田,谢泰俊.南海北部大陆边缘盆地分析与油气聚集[M].北京:北京出版社,1997:1-192.
[130]任建业,雷超.莺歌海-琼东南盆地构造-地层格架及南海动力变形分区[J].地球物理学报,2011,54(12):3303-3314.
[131]SUN Q,WU S,LUF,et al.Polygonal faults and their implications for hydrocarbon reservoirs in the southern Qiongdongnan Basin,South China Sea[J].Journal of Asian Earth Sciences,2010,39(5):470-479.
[132]王振峰.深水重要油气储层:琼东南盆地中央峡谷体系[J].沉积学报,2012,30(4):646-653.
[133]龚再升,李思田,汪集旸.南海北部大陆边缘盆地油气成藏动力学研究[M].北京:北京出版社,2004:3-45.
[134]钟志洪,李绪宣,孙珍,等.莺歌海盆地的构造反转作用及其油气勘探意义[J].热带海洋学报,2007,26(1):16-21.
[135]CLIFT P D,SUN Z.The sedimentary and tectonic evolution of the Yinggehai-Song Hong basin and the southern Hainan margin,South China Sea:implications for Tibetan uplift and monsoon intensification[J].Journal of Geophysical Research,2006,111:B06405.
[136]郭令智,钟志洪,王良书,等.莺歌海盆地周边区域构造演化[J].高校地质学报,2001,7(1):1-12.
[137]SEARLE M P.Role of the Red River Shear Zone,Yunnan and Vietnam,in the continental extrusion of SE Asia[J].Journal of the Geological Society,2006,163(6):1025-1036.
[138]殷秀兰,李思田,杨计海,等.琼西莺歌海盆地断裂系统的成因机制[J].地质通报,2002,21(10):653-657.
[139]郝芳,刘建章,邹华耀,等.莺歌海—琼东南盆地超压层系油气聚散机理浅析[J].地学前缘,2015,22(1):169-180.
[140]XIE X N,LI S T,DONG W L,et al.Overpressure development and hydrofracturing in the Yinggehai Basin,South China Sea[J].Journal of Petroleum Geology,1999,22(4):437-453.
[141]朱伟林.南海北部深水区油气地质特征[J].石油学报,2010,31(4):521-527.
[142]谢玉洪,张迎朝,李绪深,等.莺歌海盆地高温超压气藏控藏要素与成藏模式[J].石油学报,2012,33(4):601-609.
[143]张云帆,孙珍,郭兴伟,等.琼东南盆地新生代沉降特征[J].热带海洋学报,2008,27(5):30-36.
[144]刘见宝,孙珍,刘彦宾,等.琼东南盆地新生代构造研究现状及展望[J].海洋地质前沿,2012,28(4):1-9.
[145]CAO L,JIANG T,WANG Z,et al.Provenance of Upper Miocene sediments in the Yinggehai and Qiongdongnan basins,northwestern South China Sea:evidence from REE,heavy minerals and zircon U-Pb ages[J].Marine Geology,2015,361:136-146.
[146]王英民,徐强,李冬,等.南海西北部晚中新世的红河海底扇[J].科学通报,2011,56(10):781-787.
[147]CAO S,LIU J,LEISS B,et al.Oligo-Miocene shearing along the Ailao Shan-Red River shear zone:constraints from structural analysis and zircon U/Pb geochronology of magmatic rocks in the Diancang Shan massif,SE Tibet,China[J].Gondwana Research,2011,19(4):975-993.
[148]王策,梁新权,周云,等.莺歌海盆地东侧物源年龄标志的建立:来自琼西6条主要河流碎屑锆石LA-ICP-MS U-Pb年龄的研究[J].地学前缘,2015,22(4):277-289.
[149]WANG C,LIANG X,XIE Y,et al.Provenance of Upper Miocene to Quaternary sediments in the Yinggehai-Song Hong Basin,South China Sea:evidence from detrital zircon U-Pb ages[J].Marine Geology,2014,355:202-217.
[150]LIU X,ZHANG D,ZHAI S,et al.A heavy mineral viewpoint on sediment provenance and environment in the Qiongdongnan Basin[J].Acta Oceanologica Sinica,2015,34(4):41-55.
[151]谢玉洪,范彩伟.莺歌海盆地东方区黄流组储层成因新认识[J].中国海上油气,2010,22(6):355-359.
[152]YAN Y,CARTER A,PALK C,et al.Understanding sedimentation in the Song Hong-Yinggehai Basin,South China Sea[J].Geochemistry,Geophysics,Geosystems,2011,12:Q06014.
[153]王聪,李茂文,陈殿远,等.深水沉积层序与沉积演化模式典型实例:莺歌海盆地中深层黄流组[J].海相油气地质,2013,18(4):59-68.
[154]王策,梁新权,童传新,等.莺歌海盆地东北部邻区7条主要入海河流重砂矿物特征及其地质意义[J].沉积学报,2014,32(2):228-237.
[155]JIANG T,CAO L,XIE X,et al.Insights from heavy minerals and zircon U-Pb ages into the middle Miocene-Pliocene provenance evolution of the Yinggehai Basin,northwestern South China Sea[J].Sedimentary Geology,2015,327:32-42.
[156]王国芝,初凤友,王成善.中新世以来滇西高原内红河流域区的古高程反演[J].成都理工大学学报(自然科学版),2004,31(2):118-124.
[157]姚根顺,袁圣强,吴时国,等.琼东南盆地深水区双物源沉积模式及勘探前景[J].石油勘探与开发,2008,35(6):685-691.
[158]邵磊,李昂,吴国瑄,等.琼东南盆地沉积环境及物源演变特征[J].石油学报,2010,31(4):548-552.
[159]SUN Z,ZHOU D,ZHONG Z,et al.Experimental evidence for the dynamics of the formation of the Yinggehai basin,NW South China Sea[J].Tectonophysics,2003,372(1/2):41-58.
[160]田姗姗.琼东南盆地裂后期构造沉降分析及古地貌恢复[D].武汉:中国地质大学(武汉),2010:46-53.
[161]陈红汉,孙永传,叶加仁,等.莺-琼盆地的独特埋藏史[J].中国海上油气地质,1994,8(5):43-50.
[162]李亚敏,施小斌,徐辉龙,等.琼东南盆地构造沉降的时空分布及裂后期异常沉降机制[J].吉林大学学报(地球科学版),2012,42(1):47-57.
[163]佟殿君,任建业,雷超,等.琼东南盆地深水区岩石圈伸展模式及其对裂后期沉降的控制[J].地球科学:中国地质大学学报,2009,34(6):963-974.