南海西北次海盆及其邻区地壳结构和构造意义
|
摘要
西北次海盆的深部地壳结构蕴含着南海北部陆缘拉张过程的重要信息.广角反射/折射测线(OBS2006-2)长386km,是目前唯一的一条沿NEE向穿过西沙地块、并平行于西北次海盆扩张脊的深地震测线.通过射线追踪与走时模拟方法(RAYINVR),获得了OBS2006-2测线下方的速度结构.结果表明:西沙地块的沉积层厚度约为1～2km,而西北次海盆的沉积层厚度大约为2～3km;Moho界面从西沙地块的27km逐步抬升到西北次海盆的12km,Moho界面下方的速度为7.8～8.0km/s;未发现壳内高速层和低速层.在西沙地块和西北次海盆的过渡区,有着较大量的岩浆活动信息,推测与西北次海盆的初始扩张有关.OBS2006-2测线中114.5°E以西的地区为减薄的陆壳,而114.5°E以东的地区为洋壳,莫霍面在陆壳与洋壳的结合处剧烈抬升,地壳厚度明显减薄.西北次海盆的扩张脊下方可能有残余岩浆的存在.
Deep crustal structure in the northwest sub-basin contains the key information of the rifting process of the northern continental margin of the South China Sea(SCS).A 386km-long seismic profile(OBS2006-2)with wide-angle reflective and refractive ocean bottom seismometer(OBS)data was acquired across Xisha block and the Northwest sub-basin(NW sub-basin) of the SCS in NEE direction,which is the only profile hitherto parallel to the expanding ridge of the NW sub-basin.The crustal structure along OBS2006-2has been obtained by using ray-tracing simulation method(RAYINVR),which yields information on the velocities,tectonics,and geophysical properties.Our velocity structure indicates that sediment thickness increases from Xisha block(about 1-2km)to NW sub-basin(about 2-3km).Moho interface changes from typical continent margin of South China(～27km)to oceanic crust(～12km).The velocity at the top of upper mantle varies from 7.8to 8.0km/s.No high velocity layer and low velocity layer have been identified.Voluminous magmatism in transition zone between Xisha block and NW sub-basin,is possibly related to the initial extending of the NW sub-basin.The part of model in the domain of 220-370km would be of oceanic crust while the western part in the domain of 0-220km may be of thinned continental crust.Residual magma may exist under the speading ridge of the NW sub-basin deduced by the anomaly of Pn seismic phase.
Deep crustal structure in the northwest sub-basin contains the key information of the rifting process of the northern continental margin of the South China Sea(SCS).A 386km-long seismic profile(OBS2006-2)with wide-angle reflective and refractive ocean bottom seismometer(OBS)data was acquired across Xisha block and the Northwest sub-basin(NW sub-basin) of the SCS in NEE direction,which is the only profile hitherto parallel to the expanding ridge of the NW sub-basin.The crustal structure along OBS2006-2has been obtained by using ray-tracing simulation method(RAYINVR),which yields information on the velocities,tectonics,and geophysical properties.Our velocity structure indicates that sediment thickness increases from Xisha block(about 1-2km)to NW sub-basin(about 2-3km).Moho interface changes from typical continent margin of South China(～27km)to oceanic crust(～12km).The velocity at the top of upper mantle varies from 7.8to 8.0km/s.No high velocity layer and low velocity layer have been identified.Voluminous magmatism in transition zone between Xisha block and NW sub-basin,is possibly related to the initial extending of the NW sub-basin.The part of model in the domain of 220-370km would be of oceanic crust while the western part in the domain of 0-220km may be of thinned continental crust.Residual magma may exist under the speading ridge of the NW sub-basin deduced by the anomaly of Pn seismic phase.
引文
Ao,W.,Zhao,M.H.,Qiu,X.L.,et al.,2010.The correctionof shot and OBS position in the 3Dseismic experiment of the SW Indian Ocean ridge.Chinese J.Geophys.,53(12):2982-2991(in Chinese with English abstract).
Breivik,A.J.,Faleide,J.I.,Mjelde,R.,et al.,2009.Magmaproductivity and early seafloor spreading rate correla-tion on the northern Vring margin,Norway—con-straints on mantle melting.Tectonophysics,468(1-4):206-223.doi:10.1016/j.tecto.2008.09.020
Briais,A.,Patriat,P.,Tapponnier,P.,1993.Updated inter-pretation of magnetic anomalies and seafloor spreadingstages in the South China Sea:implications for the ter-tiary tectonics of Southeast Asia.J.Geophys.Res.,98(B4):6299-6328.doi:10.1029/92JB02280
Cande,S.C.,Kent,D.V.,1995.Revised calibration of thegeomagnetic polarity timescale for the Late Cretacousand Cenozoic.J.Geophys.Res.,100(B4):6093-6095.doi:10.1029/94JB03098
Clift,P.,Lin,J.,2001.Preferential mantle lithospheric ex-tension under the South China margin.Marine and Pe-troleum Geology,18(8):929-945.
Ding,W.W.,Li,M.B.,Zhao,L.H.,et al.,2009.Cenozoictectono-sedimentary characteristics and extension modelof the north-west sub-basin,South China Sea.EarthScience Frontiers,16(4):147-156(in Chinese withEnglish abstract).
Hao,T.Y.,Liu,J.H.,Song,H.B.,et al.,2002.Geophysicalevidences of some important faults in South China andadjacent marginal seas region.Progress in Geophysics,17(1):13-23(in Chinese with English abstract).
Hayes,D.E.,Nissen,S.S.,2005.The South China Sea mar-gins:implications for rifting contrasts.Earth andPlanetary Science Letters,237(3-4):601-616.doi:10.1016/j.epsl.2005.06.017
Koppers,A.A.P.,Watts,A.B.,2010.Intraplate seamountsas a window into deep earth processes.Oceanography,23(1):42-57.
Li,C.F.,Zhou,Z.Y.,Li,J.B.,et al.,2007.Structures ofthe northeasternmost South China Sea continental mar-gin and ocean basin:geophysical constraints and tecton-ic implications.Mar.Geophys.Res.,28(1):59-79.doi:10.1007/s11001-007-9014-9
Li,C.F.,Zhou,Z.Y.,Li,J.B.,et al.,2008.Magnetic zoningand seismic structure of the South China Sea Ocean ba-sin.Mar.Geophys.Res.,29:223-238.doi:10.1007/s11001-008-9059-4
Li,J.B.,Jin,X.L.,Gao,J.Y.,2002.Tectonic topography ofeastern sub-basin in later spreading.Science in China(Ser.D),32(3):239-248(in Chinese).
Li,X.Y.,Wu,Z.L.,Xue,B.,et al.,2007.Short-period autofloating ocean bottom seismometer and its operationalexperiences.Journal of Tropical Oceanography,26(5):35-39(in Chinese with English abstract).
Liu,J.H.,2000.The characteristics of seismic reflectionwaves in the middle area of the South China Sea andtheir significance.Acta Oceanologica Sinica,22(6):73-80(in Chinese with English abstract).
Minshull,T.A.,2009.Geophysical characterisation of theocean-continent transition at magma-poor rifted mar-gins.C.R.Geoscience,341(5):382-393.doi:10.1016/j.crte.2008.09.003
Nissen,S.S.,Hayes,D.E.,Buhl,P.,et al.,1995.Deep pen-etration seismic soudings across the northern margin ofthe South China Sea.J.Geophys.Res.,100(B11):22407-22433.
Qiu,X.L.,Zhou,D.,Xia,K.Y.,et al.,2000.OBH experi-ment and crustal structure of Xisha trough,South ChinaSea.Tropic Oceanology,19(2):9-18(in Chinese withEnglish abstract).
Qiu,X.L.,Ye,S.Y.,Wu,S.M.,et al.,2001.Crustal struc-ture across the Xisha trough,northwestern South ChinaSea.Tectonophysics,341:179-193.
Qiu,X.L.,Shi,X.B.,Yan,P.,et al.,2003.The deep seismicsurvey and research progress on crust structure of thenorthern South China Sea.Progress in Natural Sci-ence,13(3):231-236(in Chinese).
Qiu,X.L.,Chen,Y.,Zhu,R.X.,et al.,2007.The applica-tion of large volume airgun sources to the onshore-off-shore seismic surveys:implication of the experimentalresults in northern South China Sea.China Science Bul-letin,52(4):553-560.doi:10.1007/s11434-007-0051-1
Ruan,A.G.,Qiu,X.L.,Li,J.B.,et al.,2009.Wide apertureseismic sounding in the margin seas of China.SouthChina Journal of Seismology,29(2):10-18(in Chi-nese with English abstract).
Shi,X.B.,Zhou,D.,Zhang,Y.X.,et al.,2002.Density,thermal and rheological strutures of Xisha trough,South China Sea.Journal of Tropical Oceanography,21(2):23-31(in Chinese with English abstract).
Sun,Z.,Zhong,Z.H.,Zhou,D.,et al.,2006.Research onopening mechanism of South China Sea:from anologueevidence.Science in China(Ser.D),36(9):797-810(in Chinese).
Sun,Z.,Zhong,Z.H.,Keep,M.,et al.,2009.3Danaloguemodeling of the South China Sea:a discussion onbreakup pattern.Journal of Asian Earth Sciences,34(4):544-556.doi:10.1016/j.jseaes.2008.09.002
Wang,T.K.,Chen,M.K.,Lee,C.S.,et al.,2006.Seismicimaging of the transitional crust across the northeasternmargin of the South China Sea.Tectonophysics,412(3-4):237-254.doi:10.1016/j.tecto.2005.10.039
Watts,A.B.,Cochran,J.R,Selzer,G.,1975.Gravity anoma-lies and flexure of the lithosphere:a three-dimensionalstudy of the Great Meteor Seamount,Northeast Atlan-tic.J.Geophys.Res.,80(11):1391-4116.
Watts,A.B.,ten Brink,U.S.,Buhl,P.,et al.,1985.A mul-tichannel seismic study of lithospheric flexure acrossthe Hawaiian-Emperor seamount chain.Nature,315(9):105-111.
Wei,X.,Jia,C.Z.,Zhu,Y.J.,et al.,2010.Tectonic evolu-tion and infilling characteristics of the aborted oceanicbasin:taking Shuangfeng basin of South China Sea asan example.Acta Petrolei Sinica,31(2):173-179(inChinese with English abstract).
Wei,X.D.,Zhao,M.H.,Ruan,A.G.,et al.,2010.Identifi-cation and application of shear waves along the profileOBS2006-3in the mid-northern South China Sea.Jour-nal of Tropical Oceanography,29(5):72-80(in Chi-nese with English abstract).
Wu,S.M.,Zhou,D.,Qiu,X.L.,2001.Tectonic setting ofthe northern margin of South China Sea.GeologicalJournal of China Universities,7(4):419-426(in Chi-nese with English abstract).
Wu,Z.L.,Li,J.B.,Ruan,A.G.,et al.,2011.Crustal struc-ture of the northwestern sub-basin,South China Sea:results from a wide angle seismic experiment.Science inChina(Ser.D),41(10):1463-1476(in Chinese).
Xia,S.H.,Zhao,M.H.,Qiu,X.L.,et al.,2010.Crustalstructure in an onshore-offshore transitional zone nearHong Kong,northern South China Sea.Journal of Asi-an Earth Sciences,37(40669):460-472.doi:10.1016/j.jseaes.2009.11.004
Yan,P.,Zhou,D.,Liu,Z.S.,2001.A crustal structure pro-file across the northern continental margin of the SouthChina Sea.Tectonophysics,338(1):1-21.
Yao,B.C.,1996.Tectonic evolution of the South China Seain Cenozoic.Marine Geology &Quaternary Geology,16(2):1-12(in Chinese with English abstract).
Yao,B.C.,2002.Deformation characteristics of continentallithosphere when rifting and breaking-up.Marine Geol-ogy &Quaternary Geology,22(3):59-67(in Chinesewith English abstract).
Zelt,C.A.,Smith,R.B.,1992.Seismic traveltime inversionfor 2-D crustal velocity structure.Geophys.J.Int.,108(1):16-34.
Zhao,M.H.,Qiu,X.L.,Xia,K.Y.,et al.,2004.Onshore-offshore seismic data processing and preliminary resultsin NE South China Sea.Journal of Tropical Oceanog-raphy,23(1):58-63(in Chinese with English ab-stract).
Zhao,M.H.,Qiu,X.L.,Xu,H.L.,et al.,2006.Crustalstructure and its low 2velocity layer in transition zoneof South China.Journal of Tropical Oceanography,25(5):36-42(in Chinese with English abstract).
Zhao,M.H.,Qiu,X.L.,Xia,S.H.,et al.,2010.Seismicstructure in the northeastern South China Sea:S-wavevelocity and Vp/Vs ratios derived from three-compo-nent OBS data.Tectonophysics,480(40547):183-197.doi:10.1016/j.tecto.2009.10.004
敖威,赵明辉,丘学林,等,2010.西南印度洋中脊三维地震探测中炮点与海底地震仪的位置校正.地球物理学报,53(12):2982-2991.
丁巍伟,黎明碧,赵俐红,等,2009.南海西北次海盆新生代构造-沉积特征及伸展模式探讨.地学前缘,16(4):147-156.
郝天珧,刘建华,宋海斌,等,2002.华南及其相邻边缘海域一些重要断裂的地球物理证据.地球物理学进展,17(1):13-23.
李家彪,金翔龙,高金耀,2002.南海东部海盆晚期扩张的构造地貌研究.中国科学(D辑),32(3):239-248.
李湘云,吴振利,薛彬,等,2007.SEDIS-IV型短周期自浮式海底地震仪及应用体会.热带海洋学报26(5):35-39.
刘建华,2000.南海中部地震反射波特征及其地质解释.海洋学报,22(6):73-80.
丘学林,周蒂,夏戡原,等,2000.南海西沙海槽地壳结构的海底地震仪探测与研究.热带海洋,19(2):9-18.
丘学林,施小斌,阎贫,等,2003.南海北部地壳结构的深地震探测和研究新进展.自然科学进展,13(3):231-236.
阮爱国,丘学林,李家彪,等,2009.中国海洋深地震探测与研究进展.华南地震,29(2):10-18.
施小斌,周蒂,张毅祥,等,2002.南海西沙海槽岩石圈的密度结构与热-流变结构.热带海洋学报,21(2):23-31.
孙珍,钟志洪,周蒂,等,2006.南海的发育机制研究:相似模拟证据.中国科学(D辑),36(9):797-810.
魏喜,贾承造,祝永军,等,2010.夭折大洋盆地构造演化及充填特征探讨——以南海双峰盆地为例.石油学报,31(2):173-179.
卫小冬,赵明辉,阮爱国,等,2010.南海中北部OBS2006-3地震剖面中横波的识别与应用.热带海洋学报,29(5):72-80.
吴世敏,周蒂,丘学林,2001.南海北部陆缘的构造属性问题.高校地质学报,7(4):419-426.
吴振利,李家彪,阮爱国,等,2011.南海西北次海盆地壳结构:海底广角地震实验结果.中国科学(D辑),41(10):1463-1476.
姚伯初,1996.南海海盆新生代的构造演化史.海洋地质与第四纪地质,16(2):1-12.
姚伯初,2002.大陆岩石圈在张裂和分离时的变形模式.海洋地质与第四纪地质,22(3):59-67.
赵明辉,丘学林,夏戡原,等,2004.南海东北部海陆联测地震数据处理及初步结果.热带海洋学报,23(1):58-63.
赵明辉,丘学林,徐辉龙,等,2006.华南海陆过渡带的地壳结构与壳内低速层.热带海洋学报,25(5):36-42.
Breivik,A.J.,Faleide,J.I.,Mjelde,R.,et al.,2009.Magmaproductivity and early seafloor spreading rate correla-tion on the northern Vring margin,Norway—con-straints on mantle melting.Tectonophysics,468(1-4):206-223.doi:10.1016/j.tecto.2008.09.020
Briais,A.,Patriat,P.,Tapponnier,P.,1993.Updated inter-pretation of magnetic anomalies and seafloor spreadingstages in the South China Sea:implications for the ter-tiary tectonics of Southeast Asia.J.Geophys.Res.,98(B4):6299-6328.doi:10.1029/92JB02280
Cande,S.C.,Kent,D.V.,1995.Revised calibration of thegeomagnetic polarity timescale for the Late Cretacousand Cenozoic.J.Geophys.Res.,100(B4):6093-6095.doi:10.1029/94JB03098
Clift,P.,Lin,J.,2001.Preferential mantle lithospheric ex-tension under the South China margin.Marine and Pe-troleum Geology,18(8):929-945.
Ding,W.W.,Li,M.B.,Zhao,L.H.,et al.,2009.Cenozoictectono-sedimentary characteristics and extension modelof the north-west sub-basin,South China Sea.EarthScience Frontiers,16(4):147-156(in Chinese withEnglish abstract).
Hao,T.Y.,Liu,J.H.,Song,H.B.,et al.,2002.Geophysicalevidences of some important faults in South China andadjacent marginal seas region.Progress in Geophysics,17(1):13-23(in Chinese with English abstract).
Hayes,D.E.,Nissen,S.S.,2005.The South China Sea mar-gins:implications for rifting contrasts.Earth andPlanetary Science Letters,237(3-4):601-616.doi:10.1016/j.epsl.2005.06.017
Koppers,A.A.P.,Watts,A.B.,2010.Intraplate seamountsas a window into deep earth processes.Oceanography,23(1):42-57.
Li,C.F.,Zhou,Z.Y.,Li,J.B.,et al.,2007.Structures ofthe northeasternmost South China Sea continental mar-gin and ocean basin:geophysical constraints and tecton-ic implications.Mar.Geophys.Res.,28(1):59-79.doi:10.1007/s11001-007-9014-9
Li,C.F.,Zhou,Z.Y.,Li,J.B.,et al.,2008.Magnetic zoningand seismic structure of the South China Sea Ocean ba-sin.Mar.Geophys.Res.,29:223-238.doi:10.1007/s11001-008-9059-4
Li,J.B.,Jin,X.L.,Gao,J.Y.,2002.Tectonic topography ofeastern sub-basin in later spreading.Science in China(Ser.D),32(3):239-248(in Chinese).
Li,X.Y.,Wu,Z.L.,Xue,B.,et al.,2007.Short-period autofloating ocean bottom seismometer and its operationalexperiences.Journal of Tropical Oceanography,26(5):35-39(in Chinese with English abstract).
Liu,J.H.,2000.The characteristics of seismic reflectionwaves in the middle area of the South China Sea andtheir significance.Acta Oceanologica Sinica,22(6):73-80(in Chinese with English abstract).
Minshull,T.A.,2009.Geophysical characterisation of theocean-continent transition at magma-poor rifted mar-gins.C.R.Geoscience,341(5):382-393.doi:10.1016/j.crte.2008.09.003
Nissen,S.S.,Hayes,D.E.,Buhl,P.,et al.,1995.Deep pen-etration seismic soudings across the northern margin ofthe South China Sea.J.Geophys.Res.,100(B11):22407-22433.
Qiu,X.L.,Zhou,D.,Xia,K.Y.,et al.,2000.OBH experi-ment and crustal structure of Xisha trough,South ChinaSea.Tropic Oceanology,19(2):9-18(in Chinese withEnglish abstract).
Qiu,X.L.,Ye,S.Y.,Wu,S.M.,et al.,2001.Crustal struc-ture across the Xisha trough,northwestern South ChinaSea.Tectonophysics,341:179-193.
Qiu,X.L.,Shi,X.B.,Yan,P.,et al.,2003.The deep seismicsurvey and research progress on crust structure of thenorthern South China Sea.Progress in Natural Sci-ence,13(3):231-236(in Chinese).
Qiu,X.L.,Chen,Y.,Zhu,R.X.,et al.,2007.The applica-tion of large volume airgun sources to the onshore-off-shore seismic surveys:implication of the experimentalresults in northern South China Sea.China Science Bul-letin,52(4):553-560.doi:10.1007/s11434-007-0051-1
Ruan,A.G.,Qiu,X.L.,Li,J.B.,et al.,2009.Wide apertureseismic sounding in the margin seas of China.SouthChina Journal of Seismology,29(2):10-18(in Chi-nese with English abstract).
Shi,X.B.,Zhou,D.,Zhang,Y.X.,et al.,2002.Density,thermal and rheological strutures of Xisha trough,South China Sea.Journal of Tropical Oceanography,21(2):23-31(in Chinese with English abstract).
Sun,Z.,Zhong,Z.H.,Zhou,D.,et al.,2006.Research onopening mechanism of South China Sea:from anologueevidence.Science in China(Ser.D),36(9):797-810(in Chinese).
Sun,Z.,Zhong,Z.H.,Keep,M.,et al.,2009.3Danaloguemodeling of the South China Sea:a discussion onbreakup pattern.Journal of Asian Earth Sciences,34(4):544-556.doi:10.1016/j.jseaes.2008.09.002
Wang,T.K.,Chen,M.K.,Lee,C.S.,et al.,2006.Seismicimaging of the transitional crust across the northeasternmargin of the South China Sea.Tectonophysics,412(3-4):237-254.doi:10.1016/j.tecto.2005.10.039
Watts,A.B.,Cochran,J.R,Selzer,G.,1975.Gravity anoma-lies and flexure of the lithosphere:a three-dimensionalstudy of the Great Meteor Seamount,Northeast Atlan-tic.J.Geophys.Res.,80(11):1391-4116.
Watts,A.B.,ten Brink,U.S.,Buhl,P.,et al.,1985.A mul-tichannel seismic study of lithospheric flexure acrossthe Hawaiian-Emperor seamount chain.Nature,315(9):105-111.
Wei,X.,Jia,C.Z.,Zhu,Y.J.,et al.,2010.Tectonic evolu-tion and infilling characteristics of the aborted oceanicbasin:taking Shuangfeng basin of South China Sea asan example.Acta Petrolei Sinica,31(2):173-179(inChinese with English abstract).
Wei,X.D.,Zhao,M.H.,Ruan,A.G.,et al.,2010.Identifi-cation and application of shear waves along the profileOBS2006-3in the mid-northern South China Sea.Jour-nal of Tropical Oceanography,29(5):72-80(in Chi-nese with English abstract).
Wu,S.M.,Zhou,D.,Qiu,X.L.,2001.Tectonic setting ofthe northern margin of South China Sea.GeologicalJournal of China Universities,7(4):419-426(in Chi-nese with English abstract).
Wu,Z.L.,Li,J.B.,Ruan,A.G.,et al.,2011.Crustal struc-ture of the northwestern sub-basin,South China Sea:results from a wide angle seismic experiment.Science inChina(Ser.D),41(10):1463-1476(in Chinese).
Xia,S.H.,Zhao,M.H.,Qiu,X.L.,et al.,2010.Crustalstructure in an onshore-offshore transitional zone nearHong Kong,northern South China Sea.Journal of Asi-an Earth Sciences,37(40669):460-472.doi:10.1016/j.jseaes.2009.11.004
Yan,P.,Zhou,D.,Liu,Z.S.,2001.A crustal structure pro-file across the northern continental margin of the SouthChina Sea.Tectonophysics,338(1):1-21.
Yao,B.C.,1996.Tectonic evolution of the South China Seain Cenozoic.Marine Geology &Quaternary Geology,16(2):1-12(in Chinese with English abstract).
Yao,B.C.,2002.Deformation characteristics of continentallithosphere when rifting and breaking-up.Marine Geol-ogy &Quaternary Geology,22(3):59-67(in Chinesewith English abstract).
Zelt,C.A.,Smith,R.B.,1992.Seismic traveltime inversionfor 2-D crustal velocity structure.Geophys.J.Int.,108(1):16-34.
Zhao,M.H.,Qiu,X.L.,Xia,K.Y.,et al.,2004.Onshore-offshore seismic data processing and preliminary resultsin NE South China Sea.Journal of Tropical Oceanog-raphy,23(1):58-63(in Chinese with English ab-stract).
Zhao,M.H.,Qiu,X.L.,Xu,H.L.,et al.,2006.Crustalstructure and its low 2velocity layer in transition zoneof South China.Journal of Tropical Oceanography,25(5):36-42(in Chinese with English abstract).
Zhao,M.H.,Qiu,X.L.,Xia,S.H.,et al.,2010.Seismicstructure in the northeastern South China Sea:S-wavevelocity and Vp/Vs ratios derived from three-compo-nent OBS data.Tectonophysics,480(40547):183-197.doi:10.1016/j.tecto.2009.10.004
敖威,赵明辉,丘学林,等,2010.西南印度洋中脊三维地震探测中炮点与海底地震仪的位置校正.地球物理学报,53(12):2982-2991.
丁巍伟,黎明碧,赵俐红,等,2009.南海西北次海盆新生代构造-沉积特征及伸展模式探讨.地学前缘,16(4):147-156.
郝天珧,刘建华,宋海斌,等,2002.华南及其相邻边缘海域一些重要断裂的地球物理证据.地球物理学进展,17(1):13-23.
李家彪,金翔龙,高金耀,2002.南海东部海盆晚期扩张的构造地貌研究.中国科学(D辑),32(3):239-248.
李湘云,吴振利,薛彬,等,2007.SEDIS-IV型短周期自浮式海底地震仪及应用体会.热带海洋学报26(5):35-39.
刘建华,2000.南海中部地震反射波特征及其地质解释.海洋学报,22(6):73-80.
丘学林,周蒂,夏戡原,等,2000.南海西沙海槽地壳结构的海底地震仪探测与研究.热带海洋,19(2):9-18.
丘学林,施小斌,阎贫,等,2003.南海北部地壳结构的深地震探测和研究新进展.自然科学进展,13(3):231-236.
阮爱国,丘学林,李家彪,等,2009.中国海洋深地震探测与研究进展.华南地震,29(2):10-18.
施小斌,周蒂,张毅祥,等,2002.南海西沙海槽岩石圈的密度结构与热-流变结构.热带海洋学报,21(2):23-31.
孙珍,钟志洪,周蒂,等,2006.南海的发育机制研究:相似模拟证据.中国科学(D辑),36(9):797-810.
魏喜,贾承造,祝永军,等,2010.夭折大洋盆地构造演化及充填特征探讨——以南海双峰盆地为例.石油学报,31(2):173-179.
卫小冬,赵明辉,阮爱国,等,2010.南海中北部OBS2006-3地震剖面中横波的识别与应用.热带海洋学报,29(5):72-80.
吴世敏,周蒂,丘学林,2001.南海北部陆缘的构造属性问题.高校地质学报,7(4):419-426.
吴振利,李家彪,阮爱国,等,2011.南海西北次海盆地壳结构:海底广角地震实验结果.中国科学(D辑),41(10):1463-1476.
姚伯初,1996.南海海盆新生代的构造演化史.海洋地质与第四纪地质,16(2):1-12.
姚伯初,2002.大陆岩石圈在张裂和分离时的变形模式.海洋地质与第四纪地质,22(3):59-67.
赵明辉,丘学林,夏戡原,等,2004.南海东北部海陆联测地震数据处理及初步结果.热带海洋学报,23(1):58-63.
赵明辉,丘学林,徐辉龙,等,2006.华南海陆过渡带的地壳结构与壳内低速层.热带海洋学报,25(5):36-42.
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