[1]Horike M. Inversion of phase velocity of long period microtremors to the Swavevelocity structure down to the basement in urbanized areas [J]. J Phys Earth, 1985, 33(2): 5996. [2]冯少孔.微动勘探技术及其在土木工程中的应用[J].岩石力学与工程学报,2003,22(6):10291036. FENG Shaokong. Array microtremor survey and its application to civil engineering [J]. Chinese Journal of Rock Mechanics and Engineering,2003,22(6):10291036. [3]Park C B, Miller R D, Xia J. Multichannel analysis of surface waves [J]. Geophysics, 1999, 64(3): 800808. [4]Xia J, Miller R D, Park C B. Estimation of nearsurface shearwave velocity by inversion of Rayleigh waves [J]. Geophysics, 1999,64(3): 691700. [5]Lacoss R T, Kelly E J, Toksz M N. Estimation of seismic noise structure using arrays [J]. Geophysics, 1969, 34(1): 2138. [6]小渕卓也, 山本英和, 斎藤徳美, 等. 微動アレー探査における周波数波数スペクトル法と空間自己相関法から推定した Rayleigh 波の有効波長範囲の上限の検討[J]. 物理探査, 2002, 55(5): 363373. [7]Aki K. Space and time spectra of stationary stochastic waves, with special reference to microtremors[J]. Bulletin of the Earthquake Research Institute, University of Tokyo, 1957, 35(3): 415456. [8]Yamanaka H,Ishida H. Application of genetic algorithms to an inversion of surface wave dispersion data[J]. Bulletin of the Seismological Society of America, 1996, 86(2): 436444. |