[1] 许忠淮, 阎明,赵仲和. 由多个小震推断的华北地区构造应力场的方向 [J]. 地震学报, 1983, 5(3): 268-279. [2] 黄雨蕊,高阿甲,许忠淮 . 地震震源机制的研究应用于地震预报的探索 [J]. 地震地磁观测与研究, 1997, 18(1): 52-57. [3] 华祥文 .唐山强震前后北京、天津周围地区应力的变化过程 [J], 地震学报, 1980, 2(2): 130-145. [4] 阎明 .区域小震平均节面解的时空分析 [J]. 地震学报, 1991, 13(1): 10-20. [5] Jin A, Aki K. Observational and physical bases for the co da Q-1 precursor [A]. In Evaluation of proposed earthquake precursors(ed M . Wyss) [C]. AG U, 1991, Washing ton, D C. 33-53. [6] Cho et B, Aki K, Tsujiura M. Regional variation of the scaling law of earthquake source spectra [J]. Bull Seism Soc Am, 1978, 68: 49-79. [7] Sa to H. Temporal changes in scattering and attenuation associated with the ear th quake o ccur rence— a review of recent studies on coda waves [J]. Pure Appl Geo pfy s, 1988, 126: 465-497. [8] Jin A, Aki K.Temporal change in coda before the Tangshan earthquake of 1976 and the haichengearth quake of 1975[J]. J Geophy s Res, 1986, 91: 665-673. [9] Novelo-Casanova D A, Berg E, Hsu V , et al . Time-space variation seismic S-wave coda attenuation(Q -1) and magnitude distribution (b-values) for the Petatlanea rthquake [J]. Geo phys Reslett, 1985, 12: 789-792. [10] Peng J Y, Aki K, Lee W H K, et al . Temporal change in coda Qassociated with 1984 Ro und Valley earthquake in California [J]. J Geophys Res, 1987, 92: 3507-3536. [11] Hellweg M, Spudich P, Fletcher J B, et al . Stability of co da Q in the region of Parkfield, California: View from the U . S. Geo logical Survey Parkfield Dense Seismograph Array [J]. J Geo phys Res, 1995, 100(B2): 2089-2102. [12] Beroza G C, Cole A T, Ellsworth W L.Stability of coda wave attenuation during the Lo ma Prieta, California, earthquake sequence [J]. J Geo phy s Res, 1995, 100(B3): 3977-3987. [13] 马云生, 张天中, 张焕生. 北京及其周围地区尾波 Q 值分布特征的研究 [J]. 地震学报, 1995, 17(4): 448-458. [14] 王筱荣, 魏若萍. 用地震波参数预测地震的实践 [J]. 地震, 1997, 17(1): 75-79 . [15] Gusev A A.Temporal variations of the co da decay rate on Kamchatka: Are they real and precursory? [J]. J Geophys Res, 1997, 102(B4): 8381-8396. [16] Tselentis, G-Akis.Evidence for stability in coda Q associated with the Egion (Central Greece) earthquake of 15 June 1995[J]. Bull Sism So c Am, 1997, 87(6): 1679-1684. [17] 马云生, 黄蓉良, 张天中, 等 . 华北地区尾波 Q值分布特征及其准实时监测 [J]. 地震地磁观测与研究, 1998, 19(1A): 62-66. [18] 李清林, 张文玉. 张北6. 2级地震及晋北地区的重力场变化 [A]. 中国地震学会 . 第七次学术大会论 文摘要集[C]. 北京: 地震出版社, 1998. 106 . [19] 力武常次 . 地震预报[M]. 冯锐, 周新华译. 北京: 地震出版社, 1978. 123-128. [20] Wyss M.Second round of evaluations of proposed earthquake precusors [J]. P A GEO PH, 1997, 149: 3-16. |