引文
[1]Wang P X,Prell W,Blum P.Proceedings of the Ocean DrillingProgram,Initial Reports,Volume 184[R].Texas:Texas A&M U-niversity,2000:24-25.
[2]Wang P X,Zhao Q H,Jian Z M,et al.Thirty million year deep searecords in the South China Sea[J].Chinese Science Bulletin,2003,48(23):2 524-2 534.
[3]Li Jiaying.Quaternary diatoms from the South China Sea,Leg184,Site 1144 and their palaeoenvironmental evolution[J].Geo-logical Review,2002,48(5):542-551.[李家英.南海北部陆坡ODP 1144站位第四纪硅藻及其古环境演变[J].地质评论,2002,48(5):542-551.]
[4]Li Jian,Wang Rujian.Paleoproductivity variability of the northernSouth China Sea during the Past 1 Ma:The opal record from ODPSite 1144[J].Acta Geologica Sinica,2004,78(2):228-233.[李建,王汝建.南海北部一百万年以来的表层古生产力变化:来自ODP l144站的蛋白石记录[J].地质学报,2004,78(2):228-233.]
[5]Zheng Fan,Li Qianyu,Chen Muhong.A millennial scale Mid-Pleistocene paleoclimate record of planktonic foraminifera from thenorthern South China Sea Site 1144[J].Earth Science—Journal ofChina University of Geosciences,2006,31(6):780-786.[郑范,李前裕,陈木宏.南海北部1144站中更新世浮游有孔虫的千年尺度古气候记录[J].地球科学——中国地质大学学报,2006,31(6):780-786.]
[6]Huang Wei,Jian Zhimin,Bühring C.The Millennial-scale climatefluctuations revealed by the records of color reflectance from ODPsite 1144 in the northern South China Sea[J].Marine Geology&Quaternary Geology,2003,23(3):5-8.[黄维,翦知湣,BühringC.南海北部ODP 1144站颜色反射率揭示的千年尺度气候波动[J].海洋地质与第四纪地质,2003,23(3):5-8.]
[7]Jin Haiyan,Jian Zhimin.Paleoclimatic instability during the Mid-Pleistocene transition:Implications from foraminiferal stable isotopeat ODP Site 1144,northern South China Sea[J].Advances inEarth Science,2007,22(9):914-921.[金海燕,翦知湣.南海北部ODP 1144站中更新世气候转型期有孔虫稳定同位素古气候意义[J].地球科学进展,2007,22(9):914-921.]
[8]Wei Gangjian,Liang Xirong,Li Xianhua,et al.Major and trace el-emental compositions of the microtektites from ODP Site 1144[J].Geochimica,2002,31(1):35-42.[韦刚健,梁细荣,李献华,等.ODP 1144站钻孔沉积物中微玻璃陨石的元素地球化学特征[J].地球化学,2002,31(1):35-42.]
[9]Shao Lei,Li Xianhua,Wei Gangjian,et al.Provenance of a promi-nent sediment drift on the northern slope of the South China Sea[J].Science in China(Series D),2001,44(10):919-925.[邵磊,李献华,韦刚健,等.南海陆坡高速堆积体的物质来源[J].中国科学:D辑,2001,31(10):828-833.]
[10]Shao Lei,Li Xuejie,Geng Jianhua,et al.Deep water bottom cur-rent deposition in the northern South China Sea[J].Science inChina(Series D),2007,50(7):1 060-1 066.[邵磊,李学杰,耿建华,等.南海北部深水底流沉积作用[J].中国科学:D辑,2007,37(6):771-777.]
[11]Zhong Guangfa,Li Qianyu,Hao Hujun,et al.Current status ofdeep-water sediment wave studies and the South China Sea per-spectives[J].Advances in Earth Science,2007,22(9):907-913.[钟广法,李前裕,郝沪军,等.深水沉积物波及其在南海研究之现状[J].地球科学进展,2007,22(9):907-913.]
[12]Wood A W.A Textbook of Sound[M].New York:The MacMil-lan Co.,1955:360.
[13]Hamilton E L.Elastic properties of marine sediments[J].Journalof Geophysical Research,1971,76(2):576-604.
[14]Hamilton E L.Shear-wave velocity versus depth in marine sedi-ments:A review[J].Geophysics,1976,41(5):985-996.
[15]Hamilton E L,Bachman R T,Berger W H,et al.Acoustic andrelated properties of calcareous deep-sea sediments[J].Journal ofSedimentary Petrology,1982,52(3):733-753.
[16]Richardson M D,Briggs K B.On the use of acoustic impedancevalues to determine sediment properties[J].Proceedings of the In-stitute of Acoustics,1993,15(2):15-23.
[17]Gassmann F.Elastic waves through a packing of spheres[J].Ge-ophysics,1951,16(4):673-685.
[18]Dvorkin J,Nur A.Elasticity of high-porosity sandstone:Theoryfor two North Sea data sets[J].Geophysics,1996,61(5):1 363-1 370.
[19]Mindlin R D.Compliance of elastic bodies in contact[J].Journalof Applied Mechanics,1949,16:259-268.
[20]Hashin Z,Shtrikman S.A variational approach to the theory ofthe elastic behavior of muhiphase materials[J].Journal of Me-chanics and Physics Solids,1963,11(2):127-140.
[21]Dvorkin J,Prasad M.Elasticity of marine sediments:Rock phys-ics modeling[J].Geophysical Research Letters,1999,26(12):1 781-1 784.
[22]Ruiz F,Dvorkin J.Rock physics model for deep-sea shallow cal-careous sediment with porous grains[J].SEG Annual Meeting Ex-panded Abstracts,2007,26:1 599-1 603.
[23]Ruiz F,Dvorkin J.Sediment with porous grains:Rock-physicsmodel and application to marine carbonate and opal[J].Geophys-ics,2009,74(1):1-15.
[24]Berryman J G.Long-wavelength propagation in composite elasticmedia[J].Journal of the Acoustic Society of America,1980,68(B):1 809-1 831.
[25]Sun Y F.Core-log-seismic Integration in Hemipelagic MarineSediments on the Eastern Flank of the Juan de Fuca Ridge[R].Proceedings of the Ocean Drilling Program,Scientific Results,2000.
[26]Sun Y F.On the Foundations of the Dynamical Theory of Frac-tured Porous Media and the Gravity Variations Caused by Dilatan-cies[D].New York:Columbia University,1994.
[27]Reuss A.Berechnung der fliessgrenze von mischkristallen auf gr-und der Plastizitatsbedingungen für einkristalle[J].Zeitschrift fürAngewandte Mathematic aus Mechanik,1929,9:49-58.
[28]Voigt W.Lehrbuch der Kirstallphysik[M].Teubner,Leipzig,1928.
[29]Hill R.The elastic behavior of a crystalline aggregate[J].Pro-ceedings of the Physical Society,1952,A65(5):349-354.
[30]Biot M A.Theory of propagation of elastic waves in a fluid satu-rated porous solid.I.Low frequency range[J].Journal of the A-coustical Society of America,1956,28(2):168-178.
[31]Biot M A.Theory of propagation of elastic waves in a fluid satu-rated porous solid.II.Higher frequency range[J].Journal of theAcoustical Society of America,1956,28(2):179-191.
[32]Wan S M,Li A C,Clift P D,et al.Increased contribution of ter-rigenous supply from Taiwan to the northern South China Seasince 3Ma[J].Marine Geology,2010(278):115-121.
[33]Mavko G,Mukerji T,Dvorkin J.The Rock Physics Handbook[M].Cambridge:Cambridge University Press,1998:313-314.
[34]Chaika C.Physical Properties and Silica Diagenesis[D].Cali-fornia:Stanford University,1998.
[35]Batzle M,Wang Z J.Seismic properties of pore fluids[J].Geo-physics,1992,57(11):1 396-1 408.
[36]Alexandrov K S,Ryzhova T V.Elastic properties of rock-formingminerals II layered silicates[J].Bulletin USSR Academy of Sci-ence Geophysics,1961,9:1 165-1 168.
[37]Katahara K W.Clay mineral elastic properties[J].SEG AnnualMeeting Expanded Abstracts,1996,15:1 691-1 694.
[38]Han D H.Effects of Porosity and Clay Content on Wave Veloci-ties in Sandstones and Unconsolidated Sediments[D].Califor-nia:Stanford University,1987.
[39]Tosaya C A.Acoustical Properties of Clay Bearing Rocks[D].California:Stanford University,1982.
[40]Castagna J P,Han D H,Batzle M L.Issues in rock physics andimplications for DHI interpretation[J].The Leading Edge,1985,14:883-885.
[41]Wang Z,Wang H,Cates M E.Effective elastic properties of solidclays[J].Geophysics,2001,66(2):428-440.
[42]Vanorio T,Prasad M,Nur A.Elastic properties of dry clay miner-al aggregates,suspensions and sandstones[J].Geophysical Jour-nal International,2003,155(1):319-326.
[43]Mondol N H,Bjrlykke K,Jahren J,et al.Experimental mechani-cal compaction of clay mineral aggregates—Changes in physicalproperties of mudstones during burial[J].Marine and PetroleumGeology,2007,24(5):289-311.
[44]Mondol N H,Jahren J,Bjrlykke K,et al.Elastic properties ofclay minerals[J].The Leading Edge,2008,27(6):758-770.