[1] 冯德益, 谭爱娜, 王克芬. 近地震波速异常与地震预报[J]. 地球物理学报, 1974, 17(2): 84-98. [2] 冯锐, 庞庆衍, 傅征祥. 海城地震前后地震波速比的变化[J]. 地球物理学报, 1976, 19(4): 295-305. [3] Hanks T C, Wyss M. The use of body-wave spectra in the determination of seismic source parameters[J]. Bull Seism Soc Am, 1972, 62(2): 561-589. [4] Molnar P, Wyss M. Moments source dimensions and stress drops of shallow-focus earthquakes in the Tonga-Kermadec arc[J]. Phys Earth Planet Inter, 1972, 6: 263-278. [5] Molnar P, Tucker B,Brune J. Corner frequencies of P and S waves and models of earthquake sources[J]. Bull Seism Soc Am, 1973, 63(6): 2091-2104. [6] Masuda T, Takagi A.. Source parameter estimates for small earthquakes[J]. Sci Rep Tohoku Univ Ser 5. Geophys, 1978, 25: 39-54. [7] Fletcher J B. Spectra from high-dynamic range digital recordings of Oroville, California aftershocks and their source parameters[J]. Bull Seism Soc Am, 1980, 70: 1379-1402. [8] Silver P G. Retrieval of source-extent parameters and the interpretation of corner frequency[J]. Bull Seism Soc Am, 1983, 73: 1499-1511. [9] 陈运泰, 王妙月, 林邦惠, 等. 中小地震体波的频谱和纵、 横波拐角频率比[J]. 科学通报, 1976, 9: 414-418. [10] 赵志光, 王凌南, 陈翰明, 等. 南黄海地震系列的波谱分析(二)[J]. 地震, 1985, 4: 19-48. [11] 许健生, 尹志文. 共和地震前后中小地震的波谱变化[J]. 地震地磁观测与研究, 1998, 19(4): 30-36. [12] 张萍, 陈忠奇, 曹凤娟, 等. 岫岩5.4级地震前后拐角频率比的变化特征[J]. 四川地震, 2006, 121(4): 19-22. [13] 刘富安, 盛琰. 克拉玛依南地震波谱变化初探[J]. 高原地震, 2010, 22(3): 33-37. [14] Masuda T. Corner frequencies and Q values of P and S waves by simultaneous inversion techanique[J]. Tohoku Geophys. Journ, 1988, 31(3): 101-125. [15] Dahlen F A. On the ratio of P-wave to S-wave corner frequencies for shallow earthquake sources[J]. Bull Seism Soc Am, 1974, 64(2): 1159-1180. [16] 许健生, 尹志文, 张淑贞, 等. 天祝—古浪5.4级地震前后波谱异常特征研究[J]. 地震, 1999, 19(4): 393-398. [17] 张永久, 程万正. 用波谱分析方法研究雅江6.0级地震前后的波速变化[J]. 高原地震, 2004, 16(10): 18-25. [18] 郑秀芬, 欧阳飚, 张东宁, 等.“国家数字测震台网数据备份中心”技术系统建设及其对汶川大地震研究的数据支撑[J].地球物理学报, 2009, 52(5): 1412-1417. [19] 陈学忠, 李艳娥, 郭祥云. 河北文安MS5.1地震前首都圈及邻区震源动力学参数时空变化特征[J]. 地震, 2011, 31(4): 15-25. [20] Brune J N. Tectonic stress and spectra of seismic shear wave from earthquake[J]. J Geophys Res, 1970, 75(136): 4997-5009. [21] Archuleta R J, Cranswick E, Muller C, et al. Source parameters of the 1980 Mammoth Lakes, California, earthquakes sequence[J]. J Geophys Res, 1982, 87(B6): 4595-4607. [22] Keilis-Borok V I. On estimation of the displacement in an earthquake source and of source dimensions[J]. Ann Geofis, 1959, 12: 205-214. [23] Aki K, Richards P. Quantitative seismology: Theory and methods[M]. San Francisco, California: Freeman & Company, 1980. [24] Savage J C. Thermoelastic attenuation of elastic waves by cracks[J]. J Geophys Res, 1966b, 56: 577-592. [25] Walsh J B. Seismic wave attenuation in rock due to friction [J]. J Geophys Res, 1966, 71: 2591-2599. [26] Aki K, Chouet B. Origin of coda waves : Source, attenuation, and scattering effects[J]. J Geophys Res, 1975, 80: 3322-3342. [27] Rautian T G, Khalturin V I, Martynov V G, et al. Prelininary analysis of the spectral content of P and S waves from local earthquakes in the Gram, Tadjikistan region[J]. Bull Seism Soc Am, 1978, 68: 949-971. [28] Frankel A. The effects of attenuation and site response on the spectra of microearthquakes in the northeastern Caribbean[J]. Bull Seism Soc Am, 1982, 72: 1379-1402. [29] Butler R. C. S. McCreery, Frazer L N, et al. High-frequency seismic attenuation of oceanic P and S waves in the Western Pacific[J]. J Geophys Res, 1987, 92: 1383-1396. [30] Savage J C. Relation of corner frequency to fault dimensions[J]. J Geophys Res, 1972, 77(20): 3788-3796. [31] Whitcomb J H, et al. Earthquake prediction: variation of seismic velocities before the San Franciso Earthquakes[J]. 1973, 180(4086): 632-635. [32] 冯德益, 等. 我国西部地区一些强震及中强震前后波速异常的初步研究(二)[J]. 地球物理学报, 1977, 20(2): 115-122. [33] 盛菊琴, 宋治平, 赵书礼, 等. 数字化地震波形小震P波、 S波震源参数对比研究[J]. 地震地磁观测与研究, 2007, 28(5): 116-122. |