Citation: | LIANG LAO, LIN MEI=ht. 1988: Q-VALUE IN XINFENGJIANG RESERVOIR REGION ESTIMATED BY Q OF CODA WAVES OF LOCAL EARTHQUAKES. Acta Seismologica Sinica, 10(2): 124-136. |
[1] Aki, K., Analysis of the seismic coda earthquakes as scattered waves, J. Geophys, Res., 1969, 74, 615——631.
[2] Aki, K. and B. Chovet, Origin of coda waves: source, attenuation and scattering effects, J. Geophys. Res.,1975, 80, 3322——3342. [3] Herrmann, R. B., Q estimates using the coda of local earthquakes, Bufl. Seism. Soc, Amer., 1980, 70,447——468. [4] Singly S. and R, B. Herrmann, Regionalization of crustal coda Q in the continental Unified States, J Geophys. Res., 1983, 88, 527——538. [5] Chen, P. S., O. W, Nuttli, W. H. Ye and J. Z. Qin, Estimates of short——period Qvalues and seismic momenu from coda waves for earthquakes of the Beijing and Yunnan regions of China, Bull. Scisnz. Soc.mcr., 1984, 74, 1189——1207. [6] Rautian, T. G. and V. I. Khalturin, The use of the coda for determination of the earthquake source spectrum, Bull. Seisnz. Soc. Amen, 1978, 68, 923——948, [7] Нерсесов, И. Л., Экслериментальные Исследования сейсмической коды, Наука, 1981,издагелъство. [8] 程德利,张裕中,尾波观测与Q值分布.地震学报,1985,7,398——407, [9] 周克森,DSL一型流动地震仪的动态特性研究,西北地震学报,1984,6,80——89, [10] 周克森,熏烟记录地震仪的动态分析,华南地震.1984, 4, 7——15. [11] 秦嘉政、网荣举、用近震尾波估算昆明及其周围地区的Q值和地震矩,地球物理学报,1986,29,145一155. [12] 王妙月、杨愚源、胡毓良、李自强、陈运泰、金严、冯锐,新丰江水库地震的震源机制及其成因的初步探讨,中国科学,1976,1,55——97, [13] 周克森,用介质一仪器脉冲响应求新丰江库区Q值,地震研究,1984,7,399——410, [14] Anshu Jin and K. Aki, Temporal change in coda Q before the Tangshan earthnuake of 1976 and the Haicheng ear:hduake of 1975, J. Geoplzys. Pes., 1986, 91, 665——673.
[1] Aki, K., Analysis of the seismic coda earthquakes as scattered waves, J. Geophys, Res., 1969, 74, 615——631.
[2] Aki, K. and B. Chovet, Origin of coda waves: source, attenuation and scattering effects, J. Geophys. Res.,1975, 80, 3322——3342. [3] Herrmann, R. B., Q estimates using the coda of local earthquakes, Bufl. Seism. Soc, Amer., 1980, 70,447——468. [4] Singly S. and R, B. Herrmann, Regionalization of crustal coda Q in the continental Unified States, J Geophys. Res., 1983, 88, 527——538. [5] Chen, P. S., O. W, Nuttli, W. H. Ye and J. Z. Qin, Estimates of short——period Qvalues and seismic momenu from coda waves for earthquakes of the Beijing and Yunnan regions of China, Bull. Scisnz. Soc.mcr., 1984, 74, 1189——1207. [6] Rautian, T. G. and V. I. Khalturin, The use of the coda for determination of the earthquake source spectrum, Bull. Seisnz. Soc. Amen, 1978, 68, 923——948, [7] Нерсесов, И. Л., Экслериментальные Исследования сейсмической коды, Наука, 1981,издагелъство. [8] 程德利,张裕中,尾波观测与Q值分布.地震学报,1985,7,398——407, [9] 周克森,DSL一型流动地震仪的动态特性研究,西北地震学报,1984,6,80——89, [10] 周克森,熏烟记录地震仪的动态分析,华南地震.1984, 4, 7——15. [11] 秦嘉政、网荣举、用近震尾波估算昆明及其周围地区的Q值和地震矩,地球物理学报,1986,29,145一155. [12] 王妙月、杨愚源、胡毓良、李自强、陈运泰、金严、冯锐,新丰江水库地震的震源机制及其成因的初步探讨,中国科学,1976,1,55——97, [13] 周克森,用介质一仪器脉冲响应求新丰江库区Q值,地震研究,1984,7,399——410, [14] Anshu Jin and K. Aki, Temporal change in coda Q before the Tangshan earthnuake of 1976 and the Haicheng ear:hduake of 1975, J. Geoplzys. Pes., 1986, 91, 665——673. |
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GAO LONGSHENG, HUA ZHENGXING, LI RUIXUANcom sh advanc. 1987: ESTIMATION OF MEAN FREE PATH OF S-WAVES UNDER BEIJING AREA BY MEANS OF BOTH INTENSITY AND DECAY OF CODAS. Acta Seismologica Sinica, 9(4): 347-363. |