Q值研究动态
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摘要
随着人们观测能力的提高和观测手段的改善 ,反映地球介质特性的Q值的研究不断深化和发展。人们不仅利用天然地震波对Q值进行测量 ,还在实验室内对地震波的衰减理论和测量Q值的方法进行了研究。利用天然地震波测量Q值的主要方法有 :利用地球自由振荡资料、利用体波、利用面波和利用尾波来研究Q值。而实验室中对地震波衰减的研究为衰减机理提供了研究基础。这些研究都不断地加深了我们对于地球内部介质的特性及动力学过程的认识。
With the raising of people's observation and development of observation measures, the Q-value studies reflecting the media characteristics of the Earth are continuously deepened and developed. The Q-value studies are not only studied by the natural seismic wave, but also in the laboratory, where the attenuation theory of seismic wave and observing method of measuring Q-value are studied. The major methods of measuring Q-value by the natural earthquakes are the ones of using the data of free vibration of earth, body wave, surface wave and coda. And the attenuation studies of seismic wave in the laboratory have provided studying base for the mechanism studies. All these studies have intensified our understandings to the media properties and dynamic process in the inner earth.
With the raising of people's observation and development of observation measures, the Q-value studies reflecting the media characteristics of the Earth are continuously deepened and developed. The Q-value studies are not only studied by the natural seismic wave, but also in the laboratory, where the attenuation theory of seismic wave and observing method of measuring Q-value are studied. The major methods of measuring Q-value by the natural earthquakes are the ones of using the data of free vibration of earth, body wave, surface wave and coda. And the attenuation studies of seismic wave in the laboratory have provided studying base for the mechanism studies. All these studies have intensified our understandings to the media properties and dynamic process in the inner earth.
引文
[1]AndesongDL ,R .S .Hart.QoftheEarth[J].J .Geophys.Res.,1978,83(B12):5869-5882.
[2]AndersonDL ,ArchambeauCB .TheAnelasticityoftheEarth.[J]J.Geophys.Res.1964,69:2071-2084.
[3]AndersonDL ,BENMA ,ARCHAMBEAUCB .AttenuationofSeis micEnergyintheUpperMantle[J],J.Geophys.Res.1965,70:1441-1448.
[4]傅淑芳,徐大方.地幔瑞利面波的频散和衰减[J],地球物理学报,1985,28(2):198-207.
[5]CarpenterEW .Teleseismicsignalscalculatedforunderground,under waterandatmosphericexplosions[J].Geophys.J .1967,32:17-32.
[6]DerZA ,McelfreshTW .TheRelationshipbetweenAnelasticAttenua tionandRegionalAmplitudeAnomaliesofShort-PeriodPwavesinNorthAmerica[J].Bull.Seismic.Soc.Am.,1977,67:1303-1317.
[7]BarazangiM ,PenningtonW ,IsacksB .GlobalStudyofSeismicAttenu ationintheUpperMantlebehindIslandArcsUsingpPWaves[J].J.Geophys.Res.1975,80:1079-1092.
[8]张立敏,姚振兴.西藏高原拉萨附近介质的品质因子[J].地球物理学报,1979,22(1):299-303
[9]JordanTH ,SASpikin,Estimationoftheattenuationpoeratorformul tipleScSWaves(PaperI)[J].Geophys.Res,Letters,1977,4:167-170.
[10]ChanWW ,DerZA .AttenuationofMultipleScSinVariousPartsoftheWorld[J].Geophys.J .,1988,92:303-314.
[11]FrasierCW ,filsonJ.ADirectMeasurementofEarth’sShort-peri odAttenuationalongaTeleseismicRayPath[J].J.Geophys.Res.,1972,77:3782-3787.
[12]DouglasA ,CorbishleyDJ ,BlameyC ,MarshallPD .EstimationtheFiringDepthofUndergroundExplosions[J].Nature,1972,237:26-28.
[13]ArchambeauCB .flinnEA ,LambertDH .fineStructureoftheUp perMantle[J].J.Geophys.Res.,1969,74:5828-5865.
[14]AndersonDI,GivenJW .AbsorptionBandQModelfortheWarth[J].J.Geophys.Res.,1982,87:3893-3904.
[15]DerZA ,McelfreshTW ,AbsorptionBandQModelfortheWarth[J].J.Geophys.Res.,1982,87:3893-3904.
[16]DerZA ,LeesAC .MethodologiesforEstimatingt(f)fromShort-periodBodyWavesandRegionalVariationsoft(f)intheUnitedStates[J].Geophys.J .Int.,1985,82:125-140.
[17]DerZA ,McelfreshG ,WagnerR ,BurnettiJ.SpectralCharacteristicsofPWavesfromNuclearExplosionsandYieldEstimation[J].Bull.Seismic.Soc.Am.,1985,75:379-390.
[18]DerZA ,LeesAC ,CormierVF ,etal.frequencyDependenceofQintheMantleUnderlyingtheShieldAreasofEurasia.PartI:AnalysesofShort-andIntermediate-periodData[J].Geophys.J .Int.,1986,87:1057-1084.
[19]DerZA ,LeesAC ,Cormier,Vf.frequencyDependenceofQintheMantleUnderlyingtheShieldAreasofEurasia.PartIII:TheQModel[J].Geophys.J .Int.,1986b,87:1103-1112.
[20]Sat^oY .Attenuation,dispersion,andthewaveguideoftheGwave[J].Bull.Seismol.Soc.Am.,1958,48:231-251.
[21]SolomonSC .SeismicwaveattenuationandpartialmeltingintheuppermantleofNorthAmerica[J].J .Geophys.Res.,1972,77:1483-1502.
[22]TsaiYB ,KAki.Simultaneousdeterminationoftheseismicmomentandattenuationofseismicsurfacewaves[J].Bull.Seismol.Soc.Am.,1969,76:1393-1405.
[23]CanasJA ,BJMitchell.Lateralvariationofsurfacewaveanelasticat tenuationacrossthePacific[J].Bull.Seismol.Soc.Am.,1978,68:1637-1650.
[24]HwangHJ ,BJMitchell.Shearvelocities,Qβ,andthefrequencyde pendenceofQβinstableandtectonicallyactiveregionsfromsurfacewaveobservations[J].Geophys.J.R .Astron.Soc.,1987,90:575-613.
[25]Al-KhatibHH ,BJMitchell.UppernantleanelasticityandtectonicevolutionofthewesternUnitedStatesfromsurfacewaveattenuation[J].J .Geophys.Res.,1991,96:18,129-18,146
[26]胡家富,段永康.利用基阶面波反演地壳上地幔的Qβ结构[J].地震研究,2000,23(3):318-323.
[27]LiGuangpin,Xuguoming,GaoErgen,etal.QβtomographyunderthecrustanduppermantleineasternChina[J].ActaSeismologicaSinica,2000,13(1):84-92.
[28]洪学海,朱介寿.中国大陆地壳上地幔S波品质因子三维层析成像[J].地球物理学报,2003,46(5):642-651.
[29]YacoubNK ,BJMitchell.AttenuationofRayleighwaveamplitudesacrossEurasia[J].Bull.Seismol.Soc.Am.,1977,67:751-769.
[30]ChengCC ,MitchellBJ.CrustalQStructureintheUnitedStatesfromMulti-modesurfaceWaves[J].Bull.Seismol.Soc.Am.,1981,71:161-181.
[31]CongLianli,MitchellBJ.SeismicVelocityandQStructureoftheMiddleEastern]CrustandUpperMantlefromSurface-waveDisper sionandAttenuation[J].PureAppl.Geophys,1998,153:503-538.
[32]HerrmannRB .Qestimatesusingcodaoflocalearthquakes[J],Bull.Seism.Soc.Am.,1980,70:447-469.
[33]XieJ,OWNuttli.Interpretationofhigh-frequencycodaatlargedis tances:stochasticmodelingandmethodofinversion[J],GeophysicalJournal,1988,95:579-595.
[34]秦嘉政,荣举阚.1985年云南禄劝地震尾波Q值的某些研究[J].地震学报,1987,9(3):239-252.
[35]秦嘉政,荣举阚.禄劝地震余震序列尾波衰减特征[J].地震研究,1985,增刊:29-35.
[36]秦嘉政,李白基.用近震尾波估算昆明及其周围地区Q值和地震矩[J].地球物理学报,1986,29:145-156.
[37]秦嘉政,李白基.云南地区尾波衰减及其与地震前兆的关系[J].地震研究,1988,11(2):337-344.
[38]丛连理,胡家富,吴小平,等.中国大陆及邻近地区Lg尾波的Q值分布[J].中国科学,2002,32(8):617-624.
[39]胡家富,丛连理,吴小平,等.云南及周边地区Lg尾波Q值的分布特征[J].地球物理学报,2003,46(6):809-813.
[40]WinklerK ,NurA .Porefluidsandseismicattdenuationinlocks[J].Geophy.Res.Lett.,1979,6:1-4.
[41]徐果明.岩石的饱和度对地震波衰减的影响[J].地震地磁观测与研究,1985,6:125-127.
[42]门福录.波在饱水孔隙、弹性介质中的传播[J].地球物理学报,1965,14(3):2-6.
[43]门福录.波在饱和流体的孔隙介质中的传播问题[J].地球物理学报,1981,24(1):65-76.
[44]门福录.地震波在含水层中的弥散和耗散[J].地球物理学报,1984,27(4):64-73.
[45]杨文采.岩石的年弹性谐振Q模型[J].地球物理学报,1987,30(3):399-411.
[46]陈.地壳岩石的力学性能[M].北京:地震出版社,1988.
[47]TangXM .Awaveforminversiontechniqueformeasuringelasticwaveattenuationincylindricalbars[J].Geophysic,1992,57:854-859.
[48]TangXM .Waveforminversionofseismicvelocitiesandattenuationfromlow_frequencywavesincylindricalbars[J].Geophysics,1993,58:1525-1531.
[49]王彬,许昭永,赵晋明,等.岩石破裂孕育过程中的几种Q值变化[J].地震学报,1996,18(4):513-517.
[2]AndersonDL ,ArchambeauCB .TheAnelasticityoftheEarth.[J]J.Geophys.Res.1964,69:2071-2084.
[3]AndersonDL ,BENMA ,ARCHAMBEAUCB .AttenuationofSeis micEnergyintheUpperMantle[J],J.Geophys.Res.1965,70:1441-1448.
[4]傅淑芳,徐大方.地幔瑞利面波的频散和衰减[J],地球物理学报,1985,28(2):198-207.
[5]CarpenterEW .Teleseismicsignalscalculatedforunderground,under waterandatmosphericexplosions[J].Geophys.J .1967,32:17-32.
[6]DerZA ,McelfreshTW .TheRelationshipbetweenAnelasticAttenua tionandRegionalAmplitudeAnomaliesofShort-PeriodPwavesinNorthAmerica[J].Bull.Seismic.Soc.Am.,1977,67:1303-1317.
[7]BarazangiM ,PenningtonW ,IsacksB .GlobalStudyofSeismicAttenu ationintheUpperMantlebehindIslandArcsUsingpPWaves[J].J.Geophys.Res.1975,80:1079-1092.
[8]张立敏,姚振兴.西藏高原拉萨附近介质的品质因子[J].地球物理学报,1979,22(1):299-303
[9]JordanTH ,SASpikin,Estimationoftheattenuationpoeratorformul tipleScSWaves(PaperI)[J].Geophys.Res,Letters,1977,4:167-170.
[10]ChanWW ,DerZA .AttenuationofMultipleScSinVariousPartsoftheWorld[J].Geophys.J .,1988,92:303-314.
[11]FrasierCW ,filsonJ.ADirectMeasurementofEarth’sShort-peri odAttenuationalongaTeleseismicRayPath[J].J.Geophys.Res.,1972,77:3782-3787.
[12]DouglasA ,CorbishleyDJ ,BlameyC ,MarshallPD .EstimationtheFiringDepthofUndergroundExplosions[J].Nature,1972,237:26-28.
[13]ArchambeauCB .flinnEA ,LambertDH .fineStructureoftheUp perMantle[J].J.Geophys.Res.,1969,74:5828-5865.
[14]AndersonDI,GivenJW .AbsorptionBandQModelfortheWarth[J].J.Geophys.Res.,1982,87:3893-3904.
[15]DerZA ,McelfreshTW ,AbsorptionBandQModelfortheWarth[J].J.Geophys.Res.,1982,87:3893-3904.
[16]DerZA ,LeesAC .MethodologiesforEstimatingt(f)fromShort-periodBodyWavesandRegionalVariationsoft(f)intheUnitedStates[J].Geophys.J .Int.,1985,82:125-140.
[17]DerZA ,McelfreshG ,WagnerR ,BurnettiJ.SpectralCharacteristicsofPWavesfromNuclearExplosionsandYieldEstimation[J].Bull.Seismic.Soc.Am.,1985,75:379-390.
[18]DerZA ,LeesAC ,CormierVF ,etal.frequencyDependenceofQintheMantleUnderlyingtheShieldAreasofEurasia.PartI:AnalysesofShort-andIntermediate-periodData[J].Geophys.J .Int.,1986,87:1057-1084.
[19]DerZA ,LeesAC ,Cormier,Vf.frequencyDependenceofQintheMantleUnderlyingtheShieldAreasofEurasia.PartIII:TheQModel[J].Geophys.J .Int.,1986b,87:1103-1112.
[20]Sat^oY .Attenuation,dispersion,andthewaveguideoftheGwave[J].Bull.Seismol.Soc.Am.,1958,48:231-251.
[21]SolomonSC .SeismicwaveattenuationandpartialmeltingintheuppermantleofNorthAmerica[J].J .Geophys.Res.,1972,77:1483-1502.
[22]TsaiYB ,KAki.Simultaneousdeterminationoftheseismicmomentandattenuationofseismicsurfacewaves[J].Bull.Seismol.Soc.Am.,1969,76:1393-1405.
[23]CanasJA ,BJMitchell.Lateralvariationofsurfacewaveanelasticat tenuationacrossthePacific[J].Bull.Seismol.Soc.Am.,1978,68:1637-1650.
[24]HwangHJ ,BJMitchell.Shearvelocities,Qβ,andthefrequencyde pendenceofQβinstableandtectonicallyactiveregionsfromsurfacewaveobservations[J].Geophys.J.R .Astron.Soc.,1987,90:575-613.
[25]Al-KhatibHH ,BJMitchell.UppernantleanelasticityandtectonicevolutionofthewesternUnitedStatesfromsurfacewaveattenuation[J].J .Geophys.Res.,1991,96:18,129-18,146
[26]胡家富,段永康.利用基阶面波反演地壳上地幔的Qβ结构[J].地震研究,2000,23(3):318-323.
[27]LiGuangpin,Xuguoming,GaoErgen,etal.QβtomographyunderthecrustanduppermantleineasternChina[J].ActaSeismologicaSinica,2000,13(1):84-92.
[28]洪学海,朱介寿.中国大陆地壳上地幔S波品质因子三维层析成像[J].地球物理学报,2003,46(5):642-651.
[29]YacoubNK ,BJMitchell.AttenuationofRayleighwaveamplitudesacrossEurasia[J].Bull.Seismol.Soc.Am.,1977,67:751-769.
[30]ChengCC ,MitchellBJ.CrustalQStructureintheUnitedStatesfromMulti-modesurfaceWaves[J].Bull.Seismol.Soc.Am.,1981,71:161-181.
[31]CongLianli,MitchellBJ.SeismicVelocityandQStructureoftheMiddleEastern]CrustandUpperMantlefromSurface-waveDisper sionandAttenuation[J].PureAppl.Geophys,1998,153:503-538.
[32]HerrmannRB .Qestimatesusingcodaoflocalearthquakes[J],Bull.Seism.Soc.Am.,1980,70:447-469.
[33]XieJ,OWNuttli.Interpretationofhigh-frequencycodaatlargedis tances:stochasticmodelingandmethodofinversion[J],GeophysicalJournal,1988,95:579-595.
[34]秦嘉政,荣举阚.1985年云南禄劝地震尾波Q值的某些研究[J].地震学报,1987,9(3):239-252.
[35]秦嘉政,荣举阚.禄劝地震余震序列尾波衰减特征[J].地震研究,1985,增刊:29-35.
[36]秦嘉政,李白基.用近震尾波估算昆明及其周围地区Q值和地震矩[J].地球物理学报,1986,29:145-156.
[37]秦嘉政,李白基.云南地区尾波衰减及其与地震前兆的关系[J].地震研究,1988,11(2):337-344.
[38]丛连理,胡家富,吴小平,等.中国大陆及邻近地区Lg尾波的Q值分布[J].中国科学,2002,32(8):617-624.
[39]胡家富,丛连理,吴小平,等.云南及周边地区Lg尾波Q值的分布特征[J].地球物理学报,2003,46(6):809-813.
[40]WinklerK ,NurA .Porefluidsandseismicattdenuationinlocks[J].Geophy.Res.Lett.,1979,6:1-4.
[41]徐果明.岩石的饱和度对地震波衰减的影响[J].地震地磁观测与研究,1985,6:125-127.
[42]门福录.波在饱水孔隙、弹性介质中的传播[J].地球物理学报,1965,14(3):2-6.
[43]门福录.波在饱和流体的孔隙介质中的传播问题[J].地球物理学报,1981,24(1):65-76.
[44]门福录.地震波在含水层中的弥散和耗散[J].地球物理学报,1984,27(4):64-73.
[45]杨文采.岩石的年弹性谐振Q模型[J].地球物理学报,1987,30(3):399-411.
[46]陈.地壳岩石的力学性能[M].北京:地震出版社,1988.
[47]TangXM .Awaveforminversiontechniqueformeasuringelasticwaveattenuationincylindricalbars[J].Geophysic,1992,57:854-859.
[48]TangXM .Waveforminversionofseismicvelocitiesandattenuationfromlow_frequencywavesincylindricalbars[J].Geophysics,1993,58:1525-1531.
[49]王彬,许昭永,赵晋明,等.岩石破裂孕育过程中的几种Q值变化[J].地震学报,1996,18(4):513-517.
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