引文
[1]何家雄,夏斌,施小斌,等.世界绅士油气勘探进展与南海深水油气勘探前景[J].天然气地球科学,2006,17(6):747-752,806.[HE Jiaxiong,XIA Bin,SHI Xiaobin,et al.Prospect and progress for oil and gas in deep waters of the world,and the potential and prospect foreground for oil and gas in waters of the South China Sea[J].Natural Gas Geoscience,2006,17(6):747-752.]
[2]龚再升,李思田,谢泰俊,等.南海北部大陆边缘盆地分布与油气聚集[M].北京:科学出版社,1997.[GONG Zaisheng,LI Sitian,XIE Taijun,et al.Continental margin basin analysis and hydrocarbon accumulation of the northern South China Sea[M].Beijing:Science Press,1997.]
[3]Xie X N,Muller R D,Li S T,et al.Origin of anomalous subsidence along the Northern South China Sea margin and its relationship to dynamic topography[J].Marine and Petroleum Geology,2006,23:745-765.
[4]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.[YUAN Yusong,YANG Shuchun,HU Shengbiao,et al.Tectonic subsidence of Qiongdongnan Basin and its main control factors[J].Chinese Journal of Geophysics,2008,51(2):376-383.]
[5]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.[LI Yamin,SHI Xiaobin,XU Huilong,et al.Temporal and spatial distribution of tectonic subsidence and discussion on formation mechanism of anomalous post-rift tectonic subsidence in the Qiongdongnan Basin[J].Journal of Jilin University(Earth Science Edition),2012,42(1):47-57.]
[6]Zhao Z X,Sun Z,Wang Z F,et al.The dynamic mechanism of post-rift accelerated subsidence in Qiongdongnan Basin,northern South China[J].Mar.Geophys.Res,2013,doi:10.1007/s11001-013-9188-2.
[7]McKenzie D.Some remarks on the development of sedimentary basins[J].Earth and Planetary Science Letters,1978,40:25-32.
[8]Royden L,Keen C E.Rifting Process and Thermal Evolution of the Continental Margin of Eastern Canada determined from subsidence curves[J].Earth and Planetary Science Letters,1980,51:343-361.
[9]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.[TONG Dianjun,REN Jianye,LEI Chao,et al.Lithosphere stretching model of deep water in Qiongdongnan Basin,northern continental margin of South China Sea,and controlling of the post-rift subsidence[J].Earth Science:Journal of China University of Geosciences,2009,34(6):963-974.]
[10]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.[SUN Zhen,ZHONG Zhihong,ZHOU Di,et al.Deformation mechanism of Red River Fault zone during Cenozoic and experimental evidences related to Yinggehai Basin formation[J].Journal of Tropical Oceanography,2003,22(2):1-9.]
[11]雷超,任建业,佟殿君.南海北部洋陆转换带盆地发育动力学机制[J].地球物理学报,2013,56(4):1287-1299.[Lei C,Ren J Y,Tong D J.Geodynamics of the ocean-continent transition zone,northern margin of the South China Sea:Implications for the opening of the South China Sea[J].Chinese Journal of Geophysics,2013,56(4):1287-1299.]
[12]White N.An inverse method for determining lithospheric strain rate variations on geological timescales[J].Earth and Planetary Science Letters,1994,122:351-371.
[13]施小斌,丘学林.珠江口盆地北部坳陷带新生代以来的拉张应变速率史[C]//中国地球物理学会第22届年会论文集.成都,2006:325.[SHI Xiaobin,QUE Xuelin.The history of stretching strain rate since Cenozoic at north depressions in Zhujiangkou Basin[C]//Dissertations abstract of the 22nd CGS Annual Meeting,China,Chengdu,2006:325.]
[14]Song H B,Chen L,Zhang J,et al.A matlab program for 1D strain rate inversion[J].Computers&Geosciences,2010,36(1):16-23.
[15]钟志洪.莺琼盆地构造形成机制与油气聚集的研究[D].南京:南京大学,2000.[ZHONG Zhihong.The tectonic dynamics of the Ying-Qiong basin and oil&gas accumulation[D].Nanjing:Nanjing University,2000.]
[16]徐义刚,魏静娴,邱华宁,等.用火山岩制约南海的形成演化:初步认识与研究设想[J].科学通报,2012,57(20):1863-1878.[XU Yigang,WEI Jingxian,QIU Huaning,et al.Opening and evolution of the South China Sea constrained by studies on volcanic rocks:Preliminary results and a research design[J].Chinese Science Bulletin,2012,57(20):1863-1878.]
[17]李思田,林畅松,张启明,等.南海北部大陆边缘盆地幕式裂陷的动力过程及10Ma以来的构造事件[J].科学通报,1998,43(8):797-810.[LI Sitian,LIN Changsong,ZHANG Qiming,et al.Episodic rifting dynamics of marginal basins north of South China Sea and tectonic accidents since 10 Ma[J].Chinese Science Bulletin,1998,43(8):797-810.]
[18]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,2012.[LEI Chao.Structure and evolution of Yinggehai and Qiongdongnan Basins,South China Sea:Implications for Cenozoic tectonics in Southeast Asia[D].Wuhan:China University of Geosciences,2012.]
[19]Lebedev S,Nolet G.Upper mantle beneath southeast Asia from S velocity tomography[J].J Geophys.Res,2003,108:20-48.
[20]Montelli R,Nolet G,Dahlen F A,et al.Finite-frequency tomography reveals a variety of plumes in the mantle[J].Science,2004,303:338-343.
[21]Lei J S,Zhao D P,Steinberger B,et al.New seismic constraints on the upper mantle structure of the Hainan plume[J].Phys Earth Planet Inter,2009,173:33-50.
[22]Zhao D P.Seismic images under 60hotspots:search for mantle plumes[J].Gondwana Res,2007,12:335-355.
[23]Steckler M S,Watts A B.Subsidence of the Atlantic-Type Continental Margin off New York[J].Earth and Planetary Science Letters,1978,41:1-13.
[24]朱伟林,张功成,杨少坤,等.南海北部大陆边缘盆地天然气地质[M].北京:石油工业出版社,2007:43-59.[ZHU Weilin,ZHANG Gongcheng,YANG Shaokun,et al.The natural gas geology in continental margin basin of the northern South China Sea[M].Beijing:Petroleum Industry Press,2007:43-59.]
[25]Haq B U,Hardenbol J,Vail P R.Chronology of Fluctuating Sea Levels Since the Triassic[J].Science,1987,235:1156-1167.
[26]Powell M.An Efficient Method for Finding Minimum of Function of Several Variables Without Calculating[J].Computer,1964,1(7):155-162.
[27]Jarvis G T,McKenzie D.Sedimentary basin formation with finite extension rates[J].Earth and Planetary Science Letters,1980,48:42-52.
[28]张云帆,孙珍,周蒂,等.南海北部陆缘新生代地壳减薄特征及其动力学意义[J].中国科学(D辑),2007,37(12):1609-1616.[ZHANG Yunfan,SUN Zhen,Zhou Di,et al.The crust thinning characteristics and its dynamics meaning of northern margin of South China Sea[J].Science in China(Series D),2007,37(12):1609-1616.]
[29]Nissen S S,Hayes D E,Yao B C,et al.Gravity,heat-flow,and seismic constraints on the processes of crustal extension:northern margin of the South China Sea[J].Journal of Geophysical Research-Solid Earth,1995,100(B11):22447-22483.
[30]Qiu X L,Ye S Y,Wu S M,et al.Crustal structure across the Xisha Trough,northwestern South China Sea[J].Tectonophysics,2001,341(1-4):179-193.
[31]黄海波.南海西沙地块深部地壳结构的地震学研究[D].广州:中国科学院南海海洋研究所,2012.[HUANG Haibo.Seismological studying of the deep crustal structure on Xisha Block in the South China Sea[D].Guangzhou:South China Sea institute of oceanology Chinese Academy of Science,2012.]
[32]Reston T J.The extension discrepancy and syn-rift subsidence deficit at rifted margins[J].Petroleum Geoscience,2009,15:217-237.
[33]Zou H B,Fan Q C.U-Th isotopes in Hainan basalts:Implications for sub-asthenospheric origin of EM2 mantle end member and the dynamics of melting beneath Hainan Island[J].Lithos,2010,116:145-152.
[34]Zou H B,Zindler A,Xu X S,et al.Major and trace element,and NdSrPb isotope studies of Cenozoic basalts in SE China:mantle sources,regional variations,and tectonic significance[J].Chemical Geology,2000,171:33-47.
[35]Montelli R,Nolet G,Dahlen F A,et al.A catalogue of deep mantle plumes:New results from finite frequency tomography[J].Geochem.Geophys.Geosyst.,2006,7,Q11007,doi:10.1029/2006GC001248.
[36]Shi X B,Burov E,Leroy S,et al.Intrusion and its implication for subsidence:a case from the Baiyun sag,on the Northern margin of the South China Sea[J].Tectonophysics,2005,407:117-134.
①王万银,党炜.中国及其邻近海域重磁资料处理报告(R).西安:西安工程学院,2000.