瑞雷面波勘探的过去、现在和未来
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摘要
回顾了瑞雷面波勘探发展的历史,剖析了面波频散曲线正反演的进展及存在的问题,重点指出在石油和煤炭反射地震中,应从剔除面波转变为利用面波,并借助现有石油“大炮”反射地震资料中“有害的”瑞雷面波提取浅层地质结构信息,为反射地震静校正、近地表工程地质评价等提供物性参数,把反射地震的面波干扰变为对勘探十分有利的参数提取源,实现以强干扰面波为主要数据源的浅层结构探测,以促进瑞雷面波勘探技术的进一步发展。
This paper reviews the history of Rayleigh wave prospecting,analyzes the progress and existed problems in forward and inversion of dispersion curves.It is pointed out with emphases that the strategy should be changed from de-surface waves to adopting them in oil and coal reflection prospecting.From Rayleigh data in the existing petroleum reflection recording,the shallow geological structure information and physical parameters can be extracted,which will contribute to the static correction and the appraisal of near surface engineering geology.It is beneficial for reflection seismics to change the disturbing waves into the data sources for extracting parameters.The shallow structure information can be determined via using surface waves as main data source.The technique will promote further development of the surface wave exploration.
This paper reviews the history of Rayleigh wave prospecting,analyzes the progress and existed problems in forward and inversion of dispersion curves.It is pointed out with emphases that the strategy should be changed from de-surface waves to adopting them in oil and coal reflection prospecting.From Rayleigh data in the existing petroleum reflection recording,the shallow geological structure information and physical parameters can be extracted,which will contribute to the static correction and the appraisal of near surface engineering geology.It is beneficial for reflection seismics to change the disturbing waves into the data sources for extracting parameters.The shallow structure information can be determined via using surface waves as main data source.The technique will promote further development of the surface wave exploration.
引文
[1]Rayleigh L.On Waves Propagated Along the Plane Surfaceof an Elastic Solid[J].Proceedings of the London Math-ematic Society,1887,17:4 11.
[2]佐薇范.用GR-810激振系统进行勘探[M].日本:VIC株式会社,1986.
[3]杨成林.瑞雷波勘探[M].北京:地质出版社,1993.
[4]Stokoe K H,Nazarian S.Effectiveness of Ground Improve-ment from Spectral Analysis of Surface Waves[C]//In:Proc.8th Euro Conf On Soil Mech and Found Engrg.Cambridge:Cambridge University Press,1983.
[5]Nazarian S,Stokoe K H,Hudson W R.Use of Spectral A-nalysis of Surface Waves Method for Determination of Modu-li and Thicknesses of Pavement Systems[C]//In:NationalResearch Council.Transport Research Record No.930.Washington D C:Falmer Press,1983.
[6]刘云桢,王振东.瞬态表面波法的数据采集处理系统及其应用实例[J].物探与化探,1996,20(1):28 33.
[7]Haskell N A.The Dispersion of Surface Waves on Multilay-ered Media[J].Bull Seism Soc AM,1953,43:17 34.
[8]Knopoff L.A Matrix Method for Elastic Wave Problems[J].Bulletin of the Seismological Society of America,1964,54(1):431 438.
[9]Thrower E N.The Computation of Elastic Waves in LayeredMedia[J].Sound Vib,1965,2:210 226.
[10]Waston H T.A Note on Fast Computation of RayleighWave Dispersion in Multi-layered Half-space[J].Bull SeismSoc Am,1970,60:161 166.
[11]Abo-Zena A.Dispersion Function Computations for Unlimit-ed Frequency Values[J].Geophys J R Astron Soc,1979,58:91 105.
[12]李幼铭,束沛锰.层状介质中地震面波频散函数和体波广义反射系数的计算[J].地球物理学报,1982,25(2):130 139.
[13]牛滨华,何继善.半空间非水平层状介质瑞利面波的频散方程[J].物探与化探,1996,21(5):345 350.
[14]张碧星,兰从庆,喻明,等.分层介质中面波的能量分布[J].声学学报,1998,23(2):97 106.
[15]赵东,钟和,谭海平.点源激发瑞利波的半空间波场[J].物探与化探,1999,23(2):128 132.
[16]卓乐芳.固体—液体层分界面处的PSV型面波[J].西安工程学院学报,1999,21(3):71 73.
[17]凡友华,肖柏勋,刘家琦.层状介质中轴对称柱面瑞利面波频散函数的计算[J].地震工程与工程振动,2001,21(3):1 5.
[18]Zhang S X,Chan L S,Xia J H,et al.Anisotropy InducedDispersion Behaviors of Rayleigh Waves[J].SEG ExpandedAbstracts,2002,21:1404 1407.
[19]裴江云,吴永刚,刘英杰.近地表低速带反演[J].长春地质学院学报,1994,24(3):317 320.
[20]石耀林,金文.面波频散反演地球内部构造的遗传算法[J].地球物理学报,1995,38(2):189 198.
[21]Yamanaka H,Ishida H.Application of Genetic Algorithmsto an Inversion of Surface-Wave Dispersion Data[J].BullSeism Soc Am,1996,86(2):436A44.
[22]张碧星,肖柏勋,杨文杰,等.瑞雷波勘探中“之”字型频散曲线的形成机理及反演研究[J].地球物理学报,2000,43(4):557 567.
[23]朱良保.区域面波群速度反演的球谐函数法[J].地球物理学报,1997,40(4):503 511.
[24]Marquering H,Snieder R.Shear-wave Velocity StructureBeneath Europe,the Northeastern Atlantic and Western A-sia from Waveform Inversions Including Surface-wave ModeCoupling[J].Geophysical Journal International,1996,127(2):283 304.
[25]刘学伟,邰圣宏,何樵登.用面波反演风化层Q值—补偿风化层吸收提高分辨率[J].石油物探,1996,35(2):89 95.
[26]罗国安,杜世通.小波变换及信号重建在压制面波中的应用[J].石油地球物理勘探,1996,31(3):337 349.
[27]蒋连斌,陈道宏,高振山,等.一种去面波的新方法[J].石油地球物理勘探,1997,32(3):103 106.
[28]牛滨华,吕景贵,孙春岩,等.叠前面波干扰压制方法的研究与应用[J].现代地质,2001,15(3):326 332.
[29]曾校丰,钱荣毅,邓新生,等.油气反射波地震勘探记录中面波信息的提取[J].物探与化探,2001,25(6):443 446.
[30]王东才.综合利用地质雷达和瞬态瑞利波法进行地表静校正[J].物探装备,2001,11(2):84 88.
[31]Miller R D,Xia J H,Park C B,et al.Using MASW to MapBedrock in Olathe,Kansas[J].SEG Expanded Abstracts,1999,18:433 436.
[32]李媛媛,李庆春,丁梁波,等.二维小波变换迭代法去除地震面波[C]//中国地球物理学会编.中国地球物理.西安:西安地图出版社,2004.
[33]胥颐,刘福田,刘建华,等.中国大陆西北造山带及其毗邻盆地的地震层析成像[J].中国科学,2000,30(2):113 123.
[2]佐薇范.用GR-810激振系统进行勘探[M].日本:VIC株式会社,1986.
[3]杨成林.瑞雷波勘探[M].北京:地质出版社,1993.
[4]Stokoe K H,Nazarian S.Effectiveness of Ground Improve-ment from Spectral Analysis of Surface Waves[C]//In:Proc.8th Euro Conf On Soil Mech and Found Engrg.Cambridge:Cambridge University Press,1983.
[5]Nazarian S,Stokoe K H,Hudson W R.Use of Spectral A-nalysis of Surface Waves Method for Determination of Modu-li and Thicknesses of Pavement Systems[C]//In:NationalResearch Council.Transport Research Record No.930.Washington D C:Falmer Press,1983.
[6]刘云桢,王振东.瞬态表面波法的数据采集处理系统及其应用实例[J].物探与化探,1996,20(1):28 33.
[7]Haskell N A.The Dispersion of Surface Waves on Multilay-ered Media[J].Bull Seism Soc AM,1953,43:17 34.
[8]Knopoff L.A Matrix Method for Elastic Wave Problems[J].Bulletin of the Seismological Society of America,1964,54(1):431 438.
[9]Thrower E N.The Computation of Elastic Waves in LayeredMedia[J].Sound Vib,1965,2:210 226.
[10]Waston H T.A Note on Fast Computation of RayleighWave Dispersion in Multi-layered Half-space[J].Bull SeismSoc Am,1970,60:161 166.
[11]Abo-Zena A.Dispersion Function Computations for Unlimit-ed Frequency Values[J].Geophys J R Astron Soc,1979,58:91 105.
[12]李幼铭,束沛锰.层状介质中地震面波频散函数和体波广义反射系数的计算[J].地球物理学报,1982,25(2):130 139.
[13]牛滨华,何继善.半空间非水平层状介质瑞利面波的频散方程[J].物探与化探,1996,21(5):345 350.
[14]张碧星,兰从庆,喻明,等.分层介质中面波的能量分布[J].声学学报,1998,23(2):97 106.
[15]赵东,钟和,谭海平.点源激发瑞利波的半空间波场[J].物探与化探,1999,23(2):128 132.
[16]卓乐芳.固体—液体层分界面处的PSV型面波[J].西安工程学院学报,1999,21(3):71 73.
[17]凡友华,肖柏勋,刘家琦.层状介质中轴对称柱面瑞利面波频散函数的计算[J].地震工程与工程振动,2001,21(3):1 5.
[18]Zhang S X,Chan L S,Xia J H,et al.Anisotropy InducedDispersion Behaviors of Rayleigh Waves[J].SEG ExpandedAbstracts,2002,21:1404 1407.
[19]裴江云,吴永刚,刘英杰.近地表低速带反演[J].长春地质学院学报,1994,24(3):317 320.
[20]石耀林,金文.面波频散反演地球内部构造的遗传算法[J].地球物理学报,1995,38(2):189 198.
[21]Yamanaka H,Ishida H.Application of Genetic Algorithmsto an Inversion of Surface-Wave Dispersion Data[J].BullSeism Soc Am,1996,86(2):436A44.
[22]张碧星,肖柏勋,杨文杰,等.瑞雷波勘探中“之”字型频散曲线的形成机理及反演研究[J].地球物理学报,2000,43(4):557 567.
[23]朱良保.区域面波群速度反演的球谐函数法[J].地球物理学报,1997,40(4):503 511.
[24]Marquering H,Snieder R.Shear-wave Velocity StructureBeneath Europe,the Northeastern Atlantic and Western A-sia from Waveform Inversions Including Surface-wave ModeCoupling[J].Geophysical Journal International,1996,127(2):283 304.
[25]刘学伟,邰圣宏,何樵登.用面波反演风化层Q值—补偿风化层吸收提高分辨率[J].石油物探,1996,35(2):89 95.
[26]罗国安,杜世通.小波变换及信号重建在压制面波中的应用[J].石油地球物理勘探,1996,31(3):337 349.
[27]蒋连斌,陈道宏,高振山,等.一种去面波的新方法[J].石油地球物理勘探,1997,32(3):103 106.
[28]牛滨华,吕景贵,孙春岩,等.叠前面波干扰压制方法的研究与应用[J].现代地质,2001,15(3):326 332.
[29]曾校丰,钱荣毅,邓新生,等.油气反射波地震勘探记录中面波信息的提取[J].物探与化探,2001,25(6):443 446.
[30]王东才.综合利用地质雷达和瞬态瑞利波法进行地表静校正[J].物探装备,2001,11(2):84 88.
[31]Miller R D,Xia J H,Park C B,et al.Using MASW to MapBedrock in Olathe,Kansas[J].SEG Expanded Abstracts,1999,18:433 436.
[32]李媛媛,李庆春,丁梁波,等.二维小波变换迭代法去除地震面波[C]//中国地球物理学会编.中国地球物理.西安:西安地图出版社,2004.
[33]胥颐,刘福田,刘建华,等.中国大陆西北造山带及其毗邻盆地的地震层析成像[J].中国科学,2000,30(2):113 123.
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