| Citation: |
LIU HANXING, WANG SUYUN, SHI ZHENLIANGcom sh advance. 1989: A GROUND MOTION ATTENUATION MODEL DEPENDENT ON THE RUPTURE DIRECTION OF SEISMIC SOURCE. Acta Seismologica Sinica, 11(1): 24-37.
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[1] Boore, D. M,1983. Strong——motion seismology. Reu. Gcophys. and J'pace Phys., 21, 1308——1318.
[2] Campbell, K. W., 1985. Strong motion attenuation relations; Aten——year perspective. Eart/rguake Spectra,1, 799——804. [3] Scholl, R. E. and King, J. L., 1984. Proceedings of workshop on strong ground motion simulation and ear——thquake engineering application. A Technological Assessment, EER1, Berkeley, California. [4] BcniofF, H,1965. Mechanism and strain characteristics of the White Wolf as indicated by the aftershock sequence, Earthquake in Kern County, California during 1955. Calif. Dsv. Mines Bull., 171, 199——202. [5] McGuire, R. K., and Hanks, T. C., 1980. RMS accelerations and spectral amplitude of strong motion during the San Fernando,California earthquake. Bull. Seirm. Soc. Amer. 70, 1907——1919. [6] Archuleta, R. J., 1979. Rupture propagation effects in the Coyote Lake earthquake (abstract). E05. Traps ,Am, Geophys. Union. 60, 890. [7] Swanger, H. J., Day, S. M., Murphy, J. R. and Guzman, R., 1981. State——of——Art study concerning near——field earthquake ground motion. U. S. Nuclear Reg. Contra. NUKEG/CR——1978. [8] Bnatwright, J. and Boore, D. M., 1982. Analysis of the ground acceleration radiation by the 1980 Livermore Valley earthquake for directivity and dyhamic source characteristics. Bull. Seism. Soc. Amer. 72, 1843——1865. [9] Abrahamson, A, and Robert B. Darragh, 1985. The Morgan Hill earthquake of April 24, 1984——the 1.29g acceleration at Coyote Lake Dam: due to directiviy, a double event, or hoth. Earthquake Spectra, 1, 445——455. [10] Haskell, N, A., 1964. Total energy and energy spectral density of elastic wave radiation from propagating faults. Bull. Seism. Sac. Anzer. 54, 1811——1842. [11] Haskell, N. A., 1966. Total energy and energy spectral density of elastic wave radiation from propagating faults, 2, astatistical source model. Bull. Seism Soc. Anzer. 56, 125——140 [12] Aki, K., 1967. Sealing law of seismic spectrum J. Ceophys. Rcs., 72, 1217——1231. [13] Savage, T. C,1972. Relation of corner frequency tto fault dimension. J. Ceophyr. Res. 77, 3788——3795. [14] Faccioli, E., 1984. Measures of strong ground motion derived from a stochastic source model, Proceeding of the International School of Physics, Enrico Fermi, Earthquakes Observation, Theory and Interpretation. [15] K. Aki, 1980. Attenuation of shear——waves in the lithosphere for frequencies from 0.5——25Hz. Phys. Earth Planet.Int. 21, 50——60. [16] Hanks, T. C. and Kanamort, H 1979. A moment magnitude scale. J. Geophys. Res. 84, 2348——2350 [17] Joyner, W. B, and Boore, D. M., 1981. Peak horizontal acceleration and velocity from Strong——motion records including records from the 1979 Imperial valley, California earthquake Bull. Seism. Soc. Amer 71,2011——2038 [18] Campbell, K. W., 1981. Near——field source attenuation of peak liorizontal acceleration. Bull.Seism.Seism. Soc. Amer. 71 .2039——2070. [19] Kavazanjmn, E., H. Ecliezuria and McCanu, M. W., 1985. RMS acceleration liazard for San Franciso.Soil Dynam. Earthquake Eng., 4, 106——123. [20] Vanmarke, E. H. and Lai, S. P., 1980. Strong motion duration and RMS amplitude of earthquake records. Bull. Seism. Soc. Amen, 70, 1293——1307. [21] Bolt, B. A., Uhrammer, R. A. and Darragh, R. B,1)85. Murgan Htll earthquake of April 24, 1984 seismological aspects. Earthquake Spectra, 1, 407——415. [22] Archuleta, R. J., 1984. A faulting model for the 1979 Intpcrial Val;ev earthduake. J Geophys. Res,8 9,4559——4585. [23] Madariaga, R., 1983 High frequency radiation frc;u the dynamic e;trtlpuake fault models. ilunales Geo——physcae, 1. 17——23. [24] Upadhyay, S. K,and Annja, A. K., 1982. Azimuthal variation of acceleration spectral density near fault, VII Symp. on Earthquake Eug., 1, 89——92. [25] Weisherg, S,1980. Applied linear regression, Wiley, New York, 283. [26] Campbell, K. W., 1986. An empirical estimate of near——source gruund n,ution for a major mb: 6.8 earthquake in the Eastern United States. Bull. Seism. Soc. Amer,76, 1——17. [27] Campillo, M. and Bouchon, M., 1983. A theoretical study of the radiation from small strike——slip earthquake at close distances. Bull. Seism. Soc. Amen. 75. 81——96.
[1] Boore, D. M,1983. Strong——motion seismology. Reu. Gcophys. and J'pace Phys., 21, 1308——1318.
[2] Campbell, K. W., 1985. Strong motion attenuation relations; Aten——year perspective. Eart/rguake Spectra,1, 799——804. [3] Scholl, R. E. and King, J. L., 1984. Proceedings of workshop on strong ground motion simulation and ear——thquake engineering application. A Technological Assessment, EER1, Berkeley, California. [4] BcniofF, H,1965. Mechanism and strain characteristics of the White Wolf as indicated by the aftershock sequence, Earthquake in Kern County, California during 1955. Calif. Dsv. Mines Bull., 171, 199——202. [5] McGuire, R. K., and Hanks, T. C., 1980. RMS accelerations and spectral amplitude of strong motion during the San Fernando,California earthquake. Bull. Seirm. Soc. Amer. 70, 1907——1919. [6] Archuleta, R. J., 1979. Rupture propagation effects in the Coyote Lake earthquake (abstract). E05. Traps ,Am, Geophys. Union. 60, 890. [7] Swanger, H. J., Day, S. M., Murphy, J. R. and Guzman, R., 1981. State——of——Art study concerning near——field earthquake ground motion. U. S. Nuclear Reg. Contra. NUKEG/CR——1978. [8] Bnatwright, J. and Boore, D. M., 1982. Analysis of the ground acceleration radiation by the 1980 Livermore Valley earthquake for directivity and dyhamic source characteristics. Bull. Seism. Soc. Amer. 72, 1843——1865. [9] Abrahamson, A, and Robert B. Darragh, 1985. The Morgan Hill earthquake of April 24, 1984——the 1.29g acceleration at Coyote Lake Dam: due to directiviy, a double event, or hoth. Earthquake Spectra, 1, 445——455. [10] Haskell, N, A., 1964. Total energy and energy spectral density of elastic wave radiation from propagating faults. Bull. Seism. Sac. Anzer. 54, 1811——1842. [11] Haskell, N. A., 1966. Total energy and energy spectral density of elastic wave radiation from propagating faults, 2, astatistical source model. Bull. Seism Soc. Anzer. 56, 125——140 [12] Aki, K., 1967. Sealing law of seismic spectrum J. Ceophys. Rcs., 72, 1217——1231. [13] Savage, T. C,1972. Relation of corner frequency tto fault dimension. J. Ceophyr. Res. 77, 3788——3795. [14] Faccioli, E., 1984. Measures of strong ground motion derived from a stochastic source model, Proceeding of the International School of Physics, Enrico Fermi, Earthquakes Observation, Theory and Interpretation. [15] K. Aki, 1980. Attenuation of shear——waves in the lithosphere for frequencies from 0.5——25Hz. Phys. Earth Planet.Int. 21, 50——60. [16] Hanks, T. C. and Kanamort, H 1979. A moment magnitude scale. J. Geophys. Res. 84, 2348——2350 [17] Joyner, W. B, and Boore, D. M., 1981. Peak horizontal acceleration and velocity from Strong——motion records including records from the 1979 Imperial valley, California earthquake Bull. Seism. Soc. Amer 71,2011——2038 [18] Campbell, K. W., 1981. Near——field source attenuation of peak liorizontal acceleration. Bull.Seism.Seism. Soc. Amer. 71 .2039——2070. [19] Kavazanjmn, E., H. Ecliezuria and McCanu, M. W., 1985. RMS acceleration liazard for San Franciso.Soil Dynam. Earthquake Eng., 4, 106——123. [20] Vanmarke, E. H. and Lai, S. P., 1980. Strong motion duration and RMS amplitude of earthquake records. Bull. Seism. Soc. Amen, 70, 1293——1307. [21] Bolt, B. A., Uhrammer, R. A. and Darragh, R. B,1)85. Murgan Htll earthquake of April 24, 1984 seismological aspects. Earthquake Spectra, 1, 407——415. [22] Archuleta, R. J., 1984. A faulting model for the 1979 Intpcrial Val;ev earthduake. J Geophys. Res,8 9,4559——4585. [23] Madariaga, R., 1983 High frequency radiation frc;u the dynamic e;trtlpuake fault models. ilunales Geo——physcae, 1. 17——23. [24] Upadhyay, S. K,and Annja, A. K., 1982. Azimuthal variation of acceleration spectral density near fault, VII Symp. on Earthquake Eug., 1, 89——92. [25] Weisherg, S,1980. Applied linear regression, Wiley, New York, 283. [26] Campbell, K. W., 1986. An empirical estimate of near——source gruund n,ution for a major mb: 6.8 earthquake in the Eastern United States. Bull. Seism. Soc. Amer,76, 1——17. [27] Campillo, M. and Bouchon, M., 1983. A theoretical study of the radiation from small strike——slip earthquake at close distances. Bull. Seism. Soc. Amen. 75. 81——96. |
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