| Citation: |
CHEN PEISHANup, HU RUIHUAup2, ZHOU KUNGENup2, CHEN HAITONGuploans.com sh advancelucashadv. 1988: FAST DETERMINATION OF SURFACE WAVE MAGNITUDE M_s FROM DURATION OF CODA WAVES RECORDED BY SK SEISMOGRAPH. Acta Seismologica Sinica, 10(3): 247-256.
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[1] Btsztricsany, E. A., A new method for the determination of magnitude of earthquakes, Geofiz. Kozl., 1958.7, 69——96.
[2] Solovicv, S. L., $eismicity of Sakhalin, Bull. Earthyua JRes. Insr., Tokyo Univ., 1965, 43, 95——102, [3] Tsumura, K., Detcmination of earthquake magnitude from total duration of oscitllation, Bull. Earthqunkes Res. Inst., Tokyo Univ., 1967, 45, 7——18. [4] Lee, W. H. K., R. E, Bennet, and K. L. Meaghe:、A method of estimating magnitude of local earthquakes from signal duration, U. S. Geol. Surv., Open——Filc Rrpnrz., 1972, 28. [5] Real, C. R, and T. L. Teng, Local Richter magnitude and total signal duration in southern California,Bull. Seism. Soc. Amen, 1973, 63, 1809——1327. [6] Aki, K. Analysis of the seismic coda of local earthquakes as scattered waves, J. Geophys. Res., 1969, 74,615——631 [7] Prishan, C,U. W. Nuttli, Wenhua Ye, and Jiazheng Qin, Estimates of short——period Q values and seismie moments from coda waves for earthquakes of the Beijing and Yun——non regions of China, Bull. Seism. Soc.ilmcr., 1984, 74, 1189——1207. [8] Hanks, T. C. and H. kanamori, A moment magnitude scale, J. Geophys. Res., 1977, 84, 2348——2350. [9] 秦嘉政、陈培善,用地震波的持续时间测定川滇地区的近震震级,地震学报,1984,6,58——65, [10] 陈培善、刘祖荫、阐荣举、秦嘉政,由中小地震的震级Mt,和Ms估算197。年通海地震前后其周围地区的剪应力值,地震学报,1982,4,227——238, [11] 陈培善、胡瑞华、周坤根、李文香,面波震级的量规函数和台基校正值,地震学报,1984,6,增刊,510——524, [12] 陈培善、叶文华,论中国地震台网测得的面波震级,地球物理学报,1987,30,39——51,
[1] Btsztricsany, E. A., A new method for the determination of magnitude of earthquakes, Geofiz. Kozl., 1958.7, 69——96.
[2] Solovicv, S. L., $eismicity of Sakhalin, Bull. Earthyua JRes. Insr., Tokyo Univ., 1965, 43, 95——102, [3] Tsumura, K., Detcmination of earthquake magnitude from total duration of oscitllation, Bull. Earthqunkes Res. Inst., Tokyo Univ., 1967, 45, 7——18. [4] Lee, W. H. K., R. E, Bennet, and K. L. Meaghe:、A method of estimating magnitude of local earthquakes from signal duration, U. S. Geol. Surv., Open——Filc Rrpnrz., 1972, 28. [5] Real, C. R, and T. L. Teng, Local Richter magnitude and total signal duration in southern California,Bull. Seism. Soc. Amen, 1973, 63, 1809——1327. [6] Aki, K. Analysis of the seismic coda of local earthquakes as scattered waves, J. Geophys. Res., 1969, 74,615——631 [7] Prishan, C,U. W. Nuttli, Wenhua Ye, and Jiazheng Qin, Estimates of short——period Q values and seismie moments from coda waves for earthquakes of the Beijing and Yun——non regions of China, Bull. Seism. Soc.ilmcr., 1984, 74, 1189——1207. [8] Hanks, T. C. and H. kanamori, A moment magnitude scale, J. Geophys. Res., 1977, 84, 2348——2350. [9] 秦嘉政、陈培善,用地震波的持续时间测定川滇地区的近震震级,地震学报,1984,6,58——65, [10] 陈培善、刘祖荫、阐荣举、秦嘉政,由中小地震的震级Mt,和Ms估算197。年通海地震前后其周围地区的剪应力值,地震学报,1982,4,227——238, [11] 陈培善、胡瑞华、周坤根、李文香,面波震级的量规函数和台基校正值,地震学报,1984,6,增刊,510——524, [12] 陈培善、叶文华,论中国地震台网测得的面波震级,地球物理学报,1987,30,39——51, |
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