台阵地震学、地震台阵与禁核试条约监测系统
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摘要
本文介绍了台阵地震学的发展,国内外地震台阵的建设和工作进展以及地震台阵与全面禁止核试验条约(CTBT)国际监测系统(IMS)的关系。另外比较系统地论述了台阵地震学在地震精确定位和地球内部构造反演中的应用。
The development of array seismology was introduced,also the history and status of seismic array at home and abroad,and the relationship between seismic array and CTBT(Comprehensive Nuclear-Test-Ban Treaty)/IMS(International Monitoring System) were also introduced. Finally,the use of array seismology in locating accurately and inversion to the inner of the earth were discussed in detail.
The development of array seismology was introduced,also the history and status of seismic array at home and abroad,and the relationship between seismic array and CTBT(Comprehensive Nuclear-Test-Ban Treaty)/IMS(International Monitoring System) were also introduced. Finally,the use of array seismology in locating accurately and inversion to the inner of the earth were discussed in detail.
引文
丁志峰、曾融生,1994,用近震资料反演京津唐地区的地壳三维速度结构,华北地震科学,12(2),15~20。
郝春月、郑重,2006,信号相关性方法在西藏那曲台阵设计中的应用,中国地震,22(1),34~42。
郝春月、郑重、牟磊育,2002a,兰州台阵勘址测点对相干函数的计算与分析,地震地磁观测与研究,23(4),29~33。
郝春月、郑重、周公威,2002b,兰州台阵勘址测点的功率谱估计与分析,地震地磁观测与研究,23(3),53~58。
郝春月、郑重、周公威,2003,兰州台阵勘址测点相关值曲线的计算分析与初选台阵评估,地震学报,25(6),608~614。
潘科、蒋秀琴、卢造勋等,2001,辽宁及邻区地壳上地幔三维速度的地震层析成像,地震地磁观测与研究,22(2),92~98。
全面禁止核试验条约组织筹备委员会(CTBTO),1996,全面禁止核试验条约(禁核试条约及CTBT)。
佟玉霞、朱元清,2001,上海地震台阵的波数响应,地震学报,23(1),98~102。
万永革、刘瑞丰、李鸿吉,1997,用遗传算法反演京津唐张地区的三维地壳结构和震源位置,地震学报,19(6),623~633。
于海英、朱元清、阚道玲等,2006a,上海地震台阵标定结果研究,中国地震,22(2),190~196。
于海英、朱元清,2006b,频率—波数分析基础理论及上海地震台阵响应分析,地震研究,29(3),312~316。
张碧秀、汤永安、夏铁军,1996,聊城—荣城地壳二维速度结构——初探“泰山震”之谜,中国地震,12(2),141~146。
朱露培、曾融生、刘福田,1990,京津唐张地区地壳上地幔三维P波速度结构,地球物理学报,33(3),267~277。
朱元清、佟玉霞、宋俊高,2002,上海地震台阵的设计方法,地震地磁观测与研究,23(2),13~23。
郑重、徐智强,2000,海拉尔兰州核查地震台阵的勘址和地动噪声功率谱的计算,地震地磁观测与研究,21(6),11~18。
中国地震局监测预报司译,2006,新地震观测实践手册,北京:地震出版社。
Aki,K.,Richards P.G.,1980,Quantitative Seismology,Theory and Methods,vols.I and II,W.H.Freeman,NewYork.
Douglas,A.,Bowers D.,Marshall P.D.,et al.,1999,Putting nuclear-test monitoringtothe test,Nature,398,474~475.
Ringdal F.,Husebye E.S.,1982,Application of arrays inthe detection,location,andidentification of seismic events,Bull.Seism.Soc.Am.,72,s201~s224.
Harjes,H.-P.,Henger M.,1973,Array-Seismologie,Z.Geophs.,39,865~905.
Johannes S.,2001,Slowness Corrections-One Wayto Improve IDC Products,Pure and Applied Geophysics,158,375~396
Karason H.,R.D.van der Hilst,2001,Tomographic imaging of the lowermost mantle with differential times of refracted and diffractedcore phases(PKP,Pdiff),J.Geophys.Res.,106,6569~6587.
Koper K.D.,Pyle M.L.,Franks J.M.,2003,Constraints on aspherical core structure fromPKiKP PcPdifferential travel times,J.Geophys.Res.,108(B3),2168,doi:10.1029/2002JB001995.
Krger,F.,Baumann M.,Scherbaum F.,et al.,2001,Mid mantle scatterers near the Mariana slab detected with a double arraymethod,Geophys.Res.Lett.,28,667~670.
Laske G.and Masters G.,1997,Aglobal digital map of sediment thickness.EOS Trans.AGU,78,F483.
Mansour N.,1966,Corrections to apparent azimuths and travel-time gradients for a dipping mohorovicic discontinuity,Bulletin of theSeismological Society of America,56(2),491~509.
McFadden,P.L.,Drummond B.J.,Kravis S.,1986,The Nth-root stack:theory,applications,and examples,Geophysics,51,1879~1892.
Mooney W.D.,Laske G.,Masters G.,1998,CRUST5.1:Aglobal model at5degrees by5degrees,J.Geophys.Res.,102,727~748.
Ritter J.R.R.,Jordan M.,Christensen U.,et al.,2001,A mantle plume belowthe Eifel volcanic fields,Germany,Earth Planet,Sci.Lett.,186,7~14.
Russian Federation/United States Calibration Working Group,2000,IMS calibrationin north America and northwestern Eurasia utilizing3-Dcrustal and upper mantle velocity models to refine location of regional seismic events,Contract No.DSWA01-98-C-0032.
Sebastian R.,Edward J.G.,2004,Array Seismology Advances Researchinto Earth s Interior,EOS,85(32),305~306.
Sebastian R.,Christine T.,2002,Array seismology:Methods and applications,Reviews of Geophysics,40(3),2-1~2-27.
Yamazaki A.,Hirahara K.,1994,The thickness of upper mantle discontinuities,as inferredfromshort-period J-Array data,GeophysRes.Lett.,21,1811~1814.
Yang X.,McLaughlin K.,North R.,1998,SSSCs for regional phases at IMS stations in North America and Fennoscandia,CMRTechnical Report,CMR-98/46.
郝春月、郑重,2006,信号相关性方法在西藏那曲台阵设计中的应用,中国地震,22(1),34~42。
郝春月、郑重、牟磊育,2002a,兰州台阵勘址测点对相干函数的计算与分析,地震地磁观测与研究,23(4),29~33。
郝春月、郑重、周公威,2002b,兰州台阵勘址测点的功率谱估计与分析,地震地磁观测与研究,23(3),53~58。
郝春月、郑重、周公威,2003,兰州台阵勘址测点相关值曲线的计算分析与初选台阵评估,地震学报,25(6),608~614。
潘科、蒋秀琴、卢造勋等,2001,辽宁及邻区地壳上地幔三维速度的地震层析成像,地震地磁观测与研究,22(2),92~98。
全面禁止核试验条约组织筹备委员会(CTBTO),1996,全面禁止核试验条约(禁核试条约及CTBT)。
佟玉霞、朱元清,2001,上海地震台阵的波数响应,地震学报,23(1),98~102。
万永革、刘瑞丰、李鸿吉,1997,用遗传算法反演京津唐张地区的三维地壳结构和震源位置,地震学报,19(6),623~633。
于海英、朱元清、阚道玲等,2006a,上海地震台阵标定结果研究,中国地震,22(2),190~196。
于海英、朱元清,2006b,频率—波数分析基础理论及上海地震台阵响应分析,地震研究,29(3),312~316。
张碧秀、汤永安、夏铁军,1996,聊城—荣城地壳二维速度结构——初探“泰山震”之谜,中国地震,12(2),141~146。
朱露培、曾融生、刘福田,1990,京津唐张地区地壳上地幔三维P波速度结构,地球物理学报,33(3),267~277。
朱元清、佟玉霞、宋俊高,2002,上海地震台阵的设计方法,地震地磁观测与研究,23(2),13~23。
郑重、徐智强,2000,海拉尔兰州核查地震台阵的勘址和地动噪声功率谱的计算,地震地磁观测与研究,21(6),11~18。
中国地震局监测预报司译,2006,新地震观测实践手册,北京:地震出版社。
Aki,K.,Richards P.G.,1980,Quantitative Seismology,Theory and Methods,vols.I and II,W.H.Freeman,NewYork.
Douglas,A.,Bowers D.,Marshall P.D.,et al.,1999,Putting nuclear-test monitoringtothe test,Nature,398,474~475.
Ringdal F.,Husebye E.S.,1982,Application of arrays inthe detection,location,andidentification of seismic events,Bull.Seism.Soc.Am.,72,s201~s224.
Harjes,H.-P.,Henger M.,1973,Array-Seismologie,Z.Geophs.,39,865~905.
Johannes S.,2001,Slowness Corrections-One Wayto Improve IDC Products,Pure and Applied Geophysics,158,375~396
Karason H.,R.D.van der Hilst,2001,Tomographic imaging of the lowermost mantle with differential times of refracted and diffractedcore phases(PKP,Pdiff),J.Geophys.Res.,106,6569~6587.
Koper K.D.,Pyle M.L.,Franks J.M.,2003,Constraints on aspherical core structure fromPKiKP PcPdifferential travel times,J.Geophys.Res.,108(B3),2168,doi:10.1029/2002JB001995.
Krger,F.,Baumann M.,Scherbaum F.,et al.,2001,Mid mantle scatterers near the Mariana slab detected with a double arraymethod,Geophys.Res.Lett.,28,667~670.
Laske G.and Masters G.,1997,Aglobal digital map of sediment thickness.EOS Trans.AGU,78,F483.
Mansour N.,1966,Corrections to apparent azimuths and travel-time gradients for a dipping mohorovicic discontinuity,Bulletin of theSeismological Society of America,56(2),491~509.
McFadden,P.L.,Drummond B.J.,Kravis S.,1986,The Nth-root stack:theory,applications,and examples,Geophysics,51,1879~1892.
Mooney W.D.,Laske G.,Masters G.,1998,CRUST5.1:Aglobal model at5degrees by5degrees,J.Geophys.Res.,102,727~748.
Ritter J.R.R.,Jordan M.,Christensen U.,et al.,2001,A mantle plume belowthe Eifel volcanic fields,Germany,Earth Planet,Sci.Lett.,186,7~14.
Russian Federation/United States Calibration Working Group,2000,IMS calibrationin north America and northwestern Eurasia utilizing3-Dcrustal and upper mantle velocity models to refine location of regional seismic events,Contract No.DSWA01-98-C-0032.
Sebastian R.,Edward J.G.,2004,Array Seismology Advances Researchinto Earth s Interior,EOS,85(32),305~306.
Sebastian R.,Christine T.,2002,Array seismology:Methods and applications,Reviews of Geophysics,40(3),2-1~2-27.
Yamazaki A.,Hirahara K.,1994,The thickness of upper mantle discontinuities,as inferredfromshort-period J-Array data,GeophysRes.Lett.,21,1811~1814.
Yang X.,McLaughlin K.,North R.,1998,SSSCs for regional phases at IMS stations in North America and Fennoscandia,CMRTechnical Report,CMR-98/46.
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