地震波衰减反演研究综述
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摘要
对地震波衰减的研究经过近五十年的发展已经取得了不少进展.本文简述了地震波的衰减机制、有关衰减的基本理论以及影响地震波衰减的主要因素,重点概括了地震波衰减的反演方法,最后预测了地震衰减研究的发展趋势.
A great progress has been made in research on seismic attenuation over fifty years of development.In this paper,it summarizes attenuation principle of seismic wave,general theories on attenuation and main factors that affect seismic attenuation.The methods of inversion on seismic attenuation are emphasized.At last,the development tendency on research of seismic attenuation is forcasted.
A great progress has been made in research on seismic attenuation over fifty years of development.In this paper,it summarizes attenuation principle of seismic wave,general theories on attenuation and main factors that affect seismic attenuation.The methods of inversion on seismic attenuation are emphasized.At last,the development tendency on research of seismic attenuation is forcasted.
引文
[1]白桦,李鲲鹏.基于时频分析的地层吸收补偿[J].石油地球物理勘探,1999,34(6):642~648.
[2]Richard Bale.The impact of attenuation on the resolution ofmulticomponent sismic data.SEG international Exposition and72nd Annual Meeting.
[3]在干燥岩石与饱和岩石中地震波的衰减[J].石油物探译丛,1986.18~40.
[4]Dutta N C,Ode H.Attenuation and dispersion of compres-sional waves in fluid-filled porous rocks with partial gas satura-tion(White model)-PartⅠ:Biot theory[J].Geophysics,1979,44(11):1777~1788.
[5]Winkler K W,Amos Nur.Seismic attenuation:Effect of porefluids and frictional sliding[J].Geophysics,1982,47:1~15.
[6]Gist G A.Fluid effect on velocity and attenuation in sand-stones[J].J Acoust Soc AM,1994,1158~1173.
[7]关于衰减测量的现状概述[J].石油物探译丛.1985.3~10.
[8]席道瑛,刘斌.孔隙流体饱和砂岩的衰减与频率的相关性[J].石油地球物理勘探,1998,33(1):66~77.
[9]席道瑛,邱文亮.饱和多孔岩石的衰减与孔隙率和饱和度的关系[J].石油地球物理勘探,1997,32(2):196~201.
[10]席道瑛,刘爱文.低频条件下饱和流体砂岩的衰减研究[J].地震学报,1995,17(4):477~481.
[11]Rainner Tonn.Comparison of seven methods for the computa-tion ofQ[J].Physics of the earth and planetary interiors,1989,259~268.
[12]Liu His-ping.Effect of source specturum on seismic attenua-tion measurements[J].Geopehysics,1998,53(12):1520~1526..
[13]Blair D P.Measurement of rise times of seismic pulses in rock[J].Geophysics,1982,47(7):1047~1058.
[14]Blair D P.Rise times of attenuation seismic pulses detected inboth empty and fluid-filled cylindrical boreholes[J].Geo-physics,1984,49(4):398~410.
[15]张平节,译.由初至波波形估测Q值-理论分析[J].物理探查(日).1989,42(4).
[16]Yih Jeng,Jing-Yih Tsai,Chen Song-Hong.An improvedmethod of determining near-surfaceQ[J].Geophysics,1999,64(5):1608~1617.
[17]Jacobson R S,George G.Shor,Jr,et al.Linear inversion ofbody wave data-PartⅡ:Attenuation versus depth using spec-tral ratios[J].Geophysics,1981,46(2):152~162.
[18]Dasgupta R,Roger A.Clark.Estimation ofQfrom surfaceseismic reflection data[J].Geophysics,1998,63(6):2120~2128.
[19]Sams M,Goldberg D.The validity ofQestimates from bore-hole data using spectral ratios[J].Geophysics,1990,55(1):97~101.
[20]Patton S W.Robust and least-squares estimation of acousticattenuation from well-data[J].Geophysics,1988,53(9):1225~1232.
[21]Pujol J,Smithson S.Seismic wave attenuation in volcanicrocks from VSP[J].Geophysics,1991,56(9):1441~1455.
[22]Zhang Changjun,Ulrych T J.Estimation of quality factorsfrom CMP records[J].Geophysics,2002,67(5):1542~1547.
[23]Anderson D L,Menahen A B,Archambeau C B.Attenua-tion of seismic energy in the upper mantle[J].Journal of Ge-ophysical Research,1965,1441~1448.
[24]裴江云,陈树民.近地表Q值求取及振幅补偿[J].地球物理学进展,2001,16(4):18~22.
[25]刘学伟,邰圣宏.用面波反演风化层的Q值[J].石油物探,1996,35(2):89~95.
[26]刘学伟,邰圣宏.一种考虑噪音干扰的地表风化层Q值反演方法[J].石油地球物理勘探,1996,31(3):367~373.
[27]李淑宁,刘荣.利用VSP资料研究地层吸收衰减规律[J].石油物探,1992,38(4):114~119.
[28]De G S,Winterstein D F,et al.Comparison of P-and S-wave velocities and Q's from VSP and sonic log data[J].Gephysics,1994,59(10):1512~1529.
[29]Hauge P S.Measurements of attenuation from vertical seis-mic profiles[J].Geophysics,1981,46(11):1548~1558.
[30]Pujol J,Smithson S.Seismic wave attenuation in volcanicrocks from VSP experiments[J].Geophysics,1991,56(9):1441~1455.
[31]Youli Quan,Jerry M.Harris.Seismic attenuation tomo-graphy using the frequency shift method[J].Geophysics,1997,62(3):895~905.
[32]用振幅衰减和脉冲增宽的地震衰减层析成像[J].石油物探译丛,1994,(3):47~51.
[33]严又生,宜明理.井间地震速度和Q值联合层析成像及应用[J].石油地球物理勘探.2001,36(1):9~17.
[34]王辉,常旭,等.井间地震波衰减成像的几种方法[J].地球物理学进展,2001,16(1):104~109.
[35]王辉,常旭,等.时间域相邻道地震波衰减成像研究[J].地球物理学报,2001,44(3):396~403.
[36]Kjartansson E.ConstanQwave propagation and attenuation[J].Geophysics Research,1979,82(B7):4737~4748.
[37]Blair D P,Spathis A T.Seismic source influence in pulse at-tenuation studies[J].Geophysics Research,1984,89(B11):9253~9258.
[38]基于心迹线频移的地震衰减层析成像[J].石油物探译丛,1994,(3):57~61.
[39]赖晓玲,张先康.三维Q值层析成像研究[J].中国科学院研究生学报,2002,19(4):357~361.
[40]徐伯勋,白旭滨.地震勘探信息技术提取、分析和预测[M].北京:地质出版社,2001.
[41]凌云.大地吸收衰减分析[J].石油地球物理勘探,2001,36(1):1~8.
[42]陈培善.地震波衰减研究在我国的进展[J].地球物理学报,1994,37(1):231~241.
[43]Qing Liao,George A.McMechan Tomographic imaging ofvelocity andQ,with application to crosswell seismic datafrom the Gypsy Pilot Site,Oklahoma[J].Geophysics,1997,62(6):1804~1811.
[44]Jianghai Xia,Miller R D,et al.Feasibility of determiningQof near-surface materials from Rayleigh waves[J].SEG,2001.
[45]陆基孟.地震勘探原理(上)[M].北京:石油工业出版社,1993.
[2]Richard Bale.The impact of attenuation on the resolution ofmulticomponent sismic data.SEG international Exposition and72nd Annual Meeting.
[3]在干燥岩石与饱和岩石中地震波的衰减[J].石油物探译丛,1986.18~40.
[4]Dutta N C,Ode H.Attenuation and dispersion of compres-sional waves in fluid-filled porous rocks with partial gas satura-tion(White model)-PartⅠ:Biot theory[J].Geophysics,1979,44(11):1777~1788.
[5]Winkler K W,Amos Nur.Seismic attenuation:Effect of porefluids and frictional sliding[J].Geophysics,1982,47:1~15.
[6]Gist G A.Fluid effect on velocity and attenuation in sand-stones[J].J Acoust Soc AM,1994,1158~1173.
[7]关于衰减测量的现状概述[J].石油物探译丛.1985.3~10.
[8]席道瑛,刘斌.孔隙流体饱和砂岩的衰减与频率的相关性[J].石油地球物理勘探,1998,33(1):66~77.
[9]席道瑛,邱文亮.饱和多孔岩石的衰减与孔隙率和饱和度的关系[J].石油地球物理勘探,1997,32(2):196~201.
[10]席道瑛,刘爱文.低频条件下饱和流体砂岩的衰减研究[J].地震学报,1995,17(4):477~481.
[11]Rainner Tonn.Comparison of seven methods for the computa-tion ofQ[J].Physics of the earth and planetary interiors,1989,259~268.
[12]Liu His-ping.Effect of source specturum on seismic attenua-tion measurements[J].Geopehysics,1998,53(12):1520~1526..
[13]Blair D P.Measurement of rise times of seismic pulses in rock[J].Geophysics,1982,47(7):1047~1058.
[14]Blair D P.Rise times of attenuation seismic pulses detected inboth empty and fluid-filled cylindrical boreholes[J].Geo-physics,1984,49(4):398~410.
[15]张平节,译.由初至波波形估测Q值-理论分析[J].物理探查(日).1989,42(4).
[16]Yih Jeng,Jing-Yih Tsai,Chen Song-Hong.An improvedmethod of determining near-surfaceQ[J].Geophysics,1999,64(5):1608~1617.
[17]Jacobson R S,George G.Shor,Jr,et al.Linear inversion ofbody wave data-PartⅡ:Attenuation versus depth using spec-tral ratios[J].Geophysics,1981,46(2):152~162.
[18]Dasgupta R,Roger A.Clark.Estimation ofQfrom surfaceseismic reflection data[J].Geophysics,1998,63(6):2120~2128.
[19]Sams M,Goldberg D.The validity ofQestimates from bore-hole data using spectral ratios[J].Geophysics,1990,55(1):97~101.
[20]Patton S W.Robust and least-squares estimation of acousticattenuation from well-data[J].Geophysics,1988,53(9):1225~1232.
[21]Pujol J,Smithson S.Seismic wave attenuation in volcanicrocks from VSP[J].Geophysics,1991,56(9):1441~1455.
[22]Zhang Changjun,Ulrych T J.Estimation of quality factorsfrom CMP records[J].Geophysics,2002,67(5):1542~1547.
[23]Anderson D L,Menahen A B,Archambeau C B.Attenua-tion of seismic energy in the upper mantle[J].Journal of Ge-ophysical Research,1965,1441~1448.
[24]裴江云,陈树民.近地表Q值求取及振幅补偿[J].地球物理学进展,2001,16(4):18~22.
[25]刘学伟,邰圣宏.用面波反演风化层的Q值[J].石油物探,1996,35(2):89~95.
[26]刘学伟,邰圣宏.一种考虑噪音干扰的地表风化层Q值反演方法[J].石油地球物理勘探,1996,31(3):367~373.
[27]李淑宁,刘荣.利用VSP资料研究地层吸收衰减规律[J].石油物探,1992,38(4):114~119.
[28]De G S,Winterstein D F,et al.Comparison of P-and S-wave velocities and Q's from VSP and sonic log data[J].Gephysics,1994,59(10):1512~1529.
[29]Hauge P S.Measurements of attenuation from vertical seis-mic profiles[J].Geophysics,1981,46(11):1548~1558.
[30]Pujol J,Smithson S.Seismic wave attenuation in volcanicrocks from VSP experiments[J].Geophysics,1991,56(9):1441~1455.
[31]Youli Quan,Jerry M.Harris.Seismic attenuation tomo-graphy using the frequency shift method[J].Geophysics,1997,62(3):895~905.
[32]用振幅衰减和脉冲增宽的地震衰减层析成像[J].石油物探译丛,1994,(3):47~51.
[33]严又生,宜明理.井间地震速度和Q值联合层析成像及应用[J].石油地球物理勘探.2001,36(1):9~17.
[34]王辉,常旭,等.井间地震波衰减成像的几种方法[J].地球物理学进展,2001,16(1):104~109.
[35]王辉,常旭,等.时间域相邻道地震波衰减成像研究[J].地球物理学报,2001,44(3):396~403.
[36]Kjartansson E.ConstanQwave propagation and attenuation[J].Geophysics Research,1979,82(B7):4737~4748.
[37]Blair D P,Spathis A T.Seismic source influence in pulse at-tenuation studies[J].Geophysics Research,1984,89(B11):9253~9258.
[38]基于心迹线频移的地震衰减层析成像[J].石油物探译丛,1994,(3):57~61.
[39]赖晓玲,张先康.三维Q值层析成像研究[J].中国科学院研究生学报,2002,19(4):357~361.
[40]徐伯勋,白旭滨.地震勘探信息技术提取、分析和预测[M].北京:地质出版社,2001.
[41]凌云.大地吸收衰减分析[J].石油地球物理勘探,2001,36(1):1~8.
[42]陈培善.地震波衰减研究在我国的进展[J].地球物理学报,1994,37(1):231~241.
[43]Qing Liao,George A.McMechan Tomographic imaging ofvelocity andQ,with application to crosswell seismic datafrom the Gypsy Pilot Site,Oklahoma[J].Geophysics,1997,62(6):1804~1811.
[44]Jianghai Xia,Miller R D,et al.Feasibility of determiningQof near-surface materials from Rayleigh waves[J].SEG,2001.
[45]陆基孟.地震勘探原理(上)[M].北京:石油工业出版社,1993.
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