地球科学进展 2012, Vol. 27 Issue (3): 359-366 DOI: 10.11867/j.issn.1001-8166.2012.03.0359 |
IODP研究 |
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南海ODP1144站深海沉积牵引体的岩石物理模型研究 |
汪鹏,钟广法 |
同济大学海洋地质国家重点实验室,上海200092 |
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Applications of Rock Physics Models to the Deep-sea Sediment Drift at ODP Site 1144, Northern South China Sea |
Wang Peng, Zhong Guangfa |
Wang Peng, Zhong Guangfa |
[1]Wang P X,Prell W,Blum P. Proceedings of the Ocean Drilling Program, Initial Reports, Volume 184[R].Texas :Texas A&M University ,2000:24-25.
[2]Wang P X,Zhao Q H,Jian Z M,et al. Thirty million year deep sea records 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, Leg 184, Site 1144 and their palaeoenvironmental evolution[J].Geological 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 northern South China Sea during the Past 1 Ma:The opal record from ODP Site 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 the northern South China Sea Site 1144[J].Earth Science—Journal of China 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 climate fluctuations revealed by the records of color reflectance from ODP site 1144 in the northern South China Sea[J].Marine Geology & Quaternary Geology,2003,23(3):5-8.[黄维,翦知湣,Bühring C. 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 isotope at ODP Site 1144, northern South China Sea[J].Advances in Earth 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 elemental 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 prominent 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 current deposition in the northern South China Sea[J].Science in China(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 of deep-water sediment wave studies and the South China Sea perspectives[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 MacMillan Co.,1955:360.
[13]Hamilton E L. Elastic properties of marine sediments[J].Journal of Geophysical Research,1971,76(2):576-604.
[14]Hamilton E L. Shear-wave velocity versus depth in marine sediments: A review[J].Geophysics, 1976, 41(5):985-996.
[15]Hamilton E L, Bachman R T, Berger W H, et al. Acoustic and related properties of calcareous deep-sea sediments[J].Journal of Sedimentary Petrology,1982,52(3): 733-753.
[16]Richardson M D,Briggs K B. On the use of acoustic impedance values to determine sediment properties[J].Proceedings of the Institute of Acoustics, 1993, 15(2): 15-23.
[17]Gassmann F. Elastic waves through a packing of spheres[J].Geophysics,1951,16(4):673-685.
[18]Dvorkin J, Nur A. Elasticity of high-porosity sandstone: Theory for 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].Journal of Applied Mechanics,1949,16:259-268.
[20]Hashin Z,Shtrikman S. A variational approach to the theory of the elastic behavior of muhiphase materials[J].Journal of Mechanics and Physics Solids,1963,11(2):127-140.
[21]Dvorkin J,Prasad M. Elasticity of marine sediments: Rock physics modeling[J].Geophysical Research Letters,1999,26(12):1 781-1 784.
[22]Ruiz F,Dvorkin J. Rock physics model for deep-sea shallow calcareous sediment with porous grains[J].SEG Annual Meeting Expanded Abstracts,2007,26:1 599-1 603.
[23]Ruiz F,Dvorkin J. Sediment with porous grains: Rock-physics model and application to marine carbonate and opal[J].Geophysics,2009,74(1):1-15.
[24]Berryman J G. Long-wavelength propagation in composite elastic media[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 Marine Sediments 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 Fractured Porous Media and the Gravity Variations Caused by Dilatancies[D].New York:Columbia University,1994.
[27]Reuss A. Berechnung der fliessgrenze von mischkristallen auf grund der Plastizitatsbedingungen für einkristalle[J].Zeitschrift für Angewandte 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].Proceedings of the Physical Society,1952,A65(5):349-354.
[30]Biot M A. Theory of propagation of elastic waves in a fluid saturated porous solid. I. Low frequency range[J].Journal of the Acoustical Society of America,1956,28(2):168-178.
[31]Biot M A. Theory of propagation of elastic waves in a fluid saturated porous solid. II. Higher frequency range[J].Journal of the Acoustical Society of America,1956,28(2):179-191.
[32]Wan S M,Li A C,Clift P D,et al. Increased contribution of terrigenous supply from Taiwan to the northern South China Sea since 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]. California:Stanford University,1998.
[35]Batzle M,Wang Z J. Seismic properties of pore fluids[J].Geophysics,1992,57(11):1 396-1 408.
[36]Alexandrov K S,Ryzhova T V. Elastic properties of rock-forming minerals II layered silicates[J].Bulletin USSR Academy of Science Geophysics,1961,9:1 165-1 168.
[37]Katahara K W. Clay mineral elastic properties[J].SEG Annual Meeting Expanded Abstracts, 1996,15:1 691-1 694.
[38]Han D H. Effects of Porosity and Clay Content on Wave Velocities in Sandstones and Unconsolidated Sediments[D]. California: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 and implications for DHI interpretation[J].The Leading Edge,1985,14:883-885.
[41]Wang Z,Wang H,Cates M E. Effective elastic properties of solid clays[J].Geophysics,2001,66(2):428-440.
[42]Vanorio T,Prasad M,Nur A. Elastic properties of dry clay mineral aggregates, suspensions and sandstones[J].Geophysical Journal International,2003,155(1):319-326.
[43]Mondol N H,Bjørlykke K,Jahren J,et al. Experimental mechanical compaction of clay mineral aggregates—Changes in physical properties of mudstones during burial[J].Marine and Petroleum Geology,2007,24(5):289-311.
[44]Mondol N H,Jahren J,Bjørlykke K,et al. Elastic properties of clay minerals[J].The Leading Edge,2008,27(6):758-770. |
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