| Citation: |
GE HUANCHENG, HUNG CAIZHONG, YE PEIYUAN, Lu ZHENFEIcom mult. 1987: Lg MAGNITUDE DETERMINATION FOR THE EASTERN SIX PROVINCES OF CHINA (PART I)--DETERMINALTION METHOD AND RESULTS. Acta Seismologica Sinica, 9(1): 37-51.
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[1] Richter, C. F., An instrumental earthquake magnitude scale, Bull. Seism. Soc. Am., 25, 1——32, 1935.
[2] 中国科学院地球物理研究所,近震分析,地震出版社,271, 1977, [3] Bath, M., O. Kalhanek, T. van Eck, and R. Wahlstrom, Engineering analysis of ground motion in Smeden,Scismol. Inst. Upsala, Rep. 5——7G, 59, 1976 [4] White, R. E., A Local magnituW scale for South Australian earthquakes, Bull. Seasm. Soc. Azu,58,1041——1057, 1968. [5] Hayes, R. C., Measurement of earthquake intensity, N. Z, T. Sci. and Technol., 22, 202B——204B, 1941. [6] Baker, R. G., Preliminary study for determining magnitude from Lg, Eartlzquake Notes, 38, 23——28, 1967. [7] Baker, R. G., Determining magnitude from Lg, Bull. Seism. Soc. Am., 60, 1907——1919, 1970. [8] Nuttli, O. W., Seismic wave attenuation and magnitude relations of Eastern North America, J. Geophys.Res.. 78, 876——885, 1973. [9] Herrmann, R. B. and O. W. Nuttli, Magnitude: the relation of ML to mbLg, Berll. Seism. Soc. Am., 72,389——397, 1982. [10] Herrmann, R. B. and A. Kijko, Shortperiod lg magnitudes: instrument, attenuation, and source effects, Bull. [11] Seirm. Soc. Arn., 73, 1835——1850, 1983 [12] 葛焕称、黄才中、叶培元、陈静巧,江苏及其邻近地区Lg波的衰减和mLg的初步测定,地震地磁观测与研究,4,11——14,1983, [13] 葛焕称、黄才中、叶培元、陆振飞,"综合回归分析"与中国东部六省地区Lg波衰减的测定,地晨学报,8, 367——381,1986. [14] 陈培善、秦嘉政,量规函数、台站方位、台基及不同测量方法对近震震级ML的影响,地震学报,5,87——98,1983. [15] 葛焕称、陈静巧、黄才中、陆振飞、叶培元,苏、鲁、豫、皖地区最大震相传播特性的初步研究,地震地磁观测与研究,4,15——17, 1983,
[1] Richter, C. F., An instrumental earthquake magnitude scale, Bull. Seism. Soc. Am., 25, 1——32, 1935.
[2] 中国科学院地球物理研究所,近震分析,地震出版社,271, 1977, [3] Bath, M., O. Kalhanek, T. van Eck, and R. Wahlstrom, Engineering analysis of ground motion in Smeden,Scismol. Inst. Upsala, Rep. 5——7G, 59, 1976 [4] White, R. E., A Local magnituW scale for South Australian earthquakes, Bull. Seasm. Soc. Azu,58,1041——1057, 1968. [5] Hayes, R. C., Measurement of earthquake intensity, N. Z, T. Sci. and Technol., 22, 202B——204B, 1941. [6] Baker, R. G., Preliminary study for determining magnitude from Lg, Eartlzquake Notes, 38, 23——28, 1967. [7] Baker, R. G., Determining magnitude from Lg, Bull. Seism. Soc. Am., 60, 1907——1919, 1970. [8] Nuttli, O. W., Seismic wave attenuation and magnitude relations of Eastern North America, J. Geophys.Res.. 78, 876——885, 1973. [9] Herrmann, R. B. and O. W. Nuttli, Magnitude: the relation of ML to mbLg, Berll. Seism. Soc. Am., 72,389——397, 1982. [10] Herrmann, R. B. and A. Kijko, Shortperiod lg magnitudes: instrument, attenuation, and source effects, Bull. [11] Seirm. Soc. Arn., 73, 1835——1850, 1983 [12] 葛焕称、黄才中、叶培元、陈静巧,江苏及其邻近地区Lg波的衰减和mLg的初步测定,地震地磁观测与研究,4,11——14,1983, [13] 葛焕称、黄才中、叶培元、陆振飞,"综合回归分析"与中国东部六省地区Lg波衰减的测定,地晨学报,8, 367——381,1986. [14] 陈培善、秦嘉政,量规函数、台站方位、台基及不同测量方法对近震震级ML的影响,地震学报,5,87——98,1983. [15] 葛焕称、陈静巧、黄才中、陆振飞、叶培元,苏、鲁、豫、皖地区最大震相传播特性的初步研究,地震地磁观测与研究,4,15——17, 1983, |
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