利用天然地震研究地壳Q值的方法和进展
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摘要
从地震波衰减品质因子(Q值)的含义及其研究意义出发,介绍了国内外利用天然地震的体波、尾波、Lg波开展地壳介质品质因子Q值研究的方法和动态,阐述了各种方法的方法原理及应用范围等,并展望了利用天然地震研究介质Q值的趋势。
Starting from the definition and significance of quality factor Q value, the main methods and developments of estimating Q value by using natural seismic waves, e.g. body waves, coda waves and Lg waves have been introduced respectively, as well as its corresponding principles and application limits are explained. The prospective on the study of seismic wave attenuation by use of earthquakes is discussed.
Starting from the definition and significance of quality factor Q value, the main methods and developments of estimating Q value by using natural seismic waves, e.g. body waves, coda waves and Lg waves have been introduced respectively, as well as its corresponding principles and application limits are explained. The prospective on the study of seismic wave attenuation by use of earthquakes is discussed.
引文
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[4]Yoshimoto K,Sato H,Yoshihisa,et al.Frequency-dependent attenuation of P and S waves in the Kanto area,Japan,based on the coda-normalization method.Geophys J Int,1993,114:165-174
[5]Yoshimoto K,Sato H,Yoshihisa,et al.Frequency-dependent attenuation of high-frequency and waves in the upper crust in western Nagano,Japan.Pure Appl Geophys,1998,153:489-502
[6]Chung Tae-Woong,Sato H.Attenuation of high frequency P and S waves in the crust of south-eastern Korea.Bull Seism Soc Amer,2001,91(6):1867-1874
[7]王勤彩,刘杰,郑斯华,等.云南地区与频率有关的P波、S波衰减研究.地震学报,2005,27(6):588-597
[8]Atkinson G M,Mereu R F.The shape of ground motion attenuation curves in southeastern Canada.Bull Seism Soc Amer,1992,82(5):2014-2031
[9]黄玉龙,郑斯华,刘杰,等.广东地区地震动衰减和场地响应的研究.地球物理学报,2003,46(1):54-61
[10]刘杰,郑斯华,黄玉龙.利用遗传算法反演非弹性衰减系数、震源系数和场地响应.地震学报,2003,25(2):211-218
[11]啜永清,苏燕,贾建喜,等.山西地区非弹性衰减系数、场地响应和几种震源参数的研究.地震学报,2004,26(4):369-378
[12]高立新,郑斯华,丁风和.内蒙古中西部地区中小地震震源参数反演和相互关系探讨.地震研究,2004,27(4):296-300
[13]赵翠萍,张智强,夏爱国,等.利用数字地震波资料研究新疆天山中东段地区的介质衰减特征.防灾减灾工程学报,2004,24(3):300-305
[14]王勤彩,高景春,郑斯华,等.华北中北部地面运动衰减研究.防灾减灾工程学报,2004,24(3):313-319
[15]刘红桂,缪发军,吴晶.场地响应、震源参数与介质衰减的同时反演.地震,2004,24(4):27-36
[16]邹振轩.浙江地区地震波衰减和场地响应研究.地震地磁观测与研究,2005,26(6):9-16
[17]李祖宁,周峥嵘,林树,等.利用数字地震台网资料联合反演福建地区Q值、场地响应和震源参数.地震地质,2005,27(3):437-445
[18]刘丽芳,刘杰,苏有锦,等.2001年施甸群非弹性衰减及震源参数特征研究.中国地震,2005,21(4):475-485
[19]刘红桂,啜永清,陈书清,等.鄂尔多斯地块地壳内S波衰减特征的研究.地震学报,2005,27(5):488-497
[20]兰从欣,刘杰,郑斯华,等.北京地区中小地震震源参数反演.地震学报,2005,27(5):498-507
[21]沈小七,刘杰,陈宇卫,等.安徽地区地震波衰减、场地响应及震源新参数的测定.地震地磁观测与研究,2005,26(3):1-10
[22]乔慧珍,张永久,程万正,等.川西北地区介质衰减特征研究.地震地磁观测与研究,2006,27(4):1-7
[23]苏有锦,刘杰,郑斯华,等.云南地区S波非弹性衰减Q值研究.地震学报,2006,28(2):206-212
[24]Young,C,Ward R W.Three-dimensionalQ-1model of the Coso hot springs known geothermal resource area.J Geophys Res,1980,85:2459-2470
[25]Evans J R,Zucca J J.Active high-resolution seismic tomography of compressional wave velocity and attenua-tion structure at Medicine Lake volcano,northern California Cascade Range.J Geophys Res,1988,93:15016-15036
[26]Clawson S R,Smith R B,Bend HM.P wave attenuation of the Yellowstone caldera from three-dimension in-version of spectral decay using explosion source seismic data.J Geophys Res,1989,94(B6):7205-7222
[27]Scherbaum F,Wyss M.Distribution of attenuation in the Kaoiki,Hawaii,Source volume estimated by inver-sion ofPwave spectra.J Geophys Res,1990,95(B8):12439-12448
[28]Lees J M,Lindley G T.Three dimensional attenuation tomography at Loma Priete,Inversion of forQ.J Geo-phys Res,1994,99(134):6843-6863
[29]Gori D,Chiarabba P C,Patane D.QPstructure of Mount Etna:Constrains for the physics of the plumbing sys-tem.J Geophys Res,2005,110,B05303,doi:10.1029/2003JB002875
[30]Hauksson E,Shearer P M.Attenuation model(QPandQS)in three dimensions of the southern California crust:Inferred fluid saturation at seismogenic depths Ho-Liu,P,HKanamori,R W Clayton,1988,Applica-tions of attenuation tomography to Imperial Valley and Coso-Indian Wells Region,southern California.J Geo-phys Res,2006,93:10501-10521
[31]赖晓玲,张先康,李松林.伽师近场地震资料处理-三维速度成像.中国科学院研究生院学报,2003,20(1):50-55
[32]王伟君,陈凌,陈棋福,等.2003年大姚地震震中区的速度和衰减结构.地球物理学报,2006,50(3):770-779
[33]Hanks TC,Wyss M.The use of body wave spectra in the determination of seismic source parameters.Bull Seism Soc Amer,1972,62,561-589
[34]Boatwright J.Detailed spectral analysis of two small NewYork State earthquake.Bull Seism Soc Amer,1978,68:1117-1131
[35]Brune J N.Tectonic stress and spectra of seismic shear wave from earthquake.J Geophys Res,1970,75(136):4997-5009
[36]Aki K.Analysis of seismic coda of local earthquakes as scatter waves.J Geophys Res,1969,74:615-631
[37]Aki K,Chouet B.Origin of coda waves,source,attenuation,and scattering effects.J Geophys Res,1975,80:3322-3342
[38]Sato H.Energy propagation including scattering effects,single isotropic scattering approximation.J Geophys Res,1977,25:27-41
[39]Chouet B,Aki K,Tsujiura M.Regional variation of the scaling law of earthquake source spectra.Bull Seism Soc Amer,1978,68:49-79
[40]Jin A,Aki K.Spatial and temporal correlation between codaQ-1and seismicity and its physical mechanism.J Geophys Res,1989,94:14041-14059
[41]Jin A,Aki K.Tempera correlation between codaQ-1and seismicity-evidence for a structural unit in the brittle-ductile transition zone.J Geodynamics,1993,17:95-120
[42]Sato H.Temporal changes in scattering and attenuation associated with the earthquake occurrence a re-view of recent studies on coda waves.Pure Appl Geophys,1988,126:465-497
[43]Singh S,Herrmann R B.Regionalization of crustal coda in the continental United States.J Geophys Res,1983,88:527-538
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