| Citation: |
Junji Koyamaup, Sihua Zhengup2com . 1991: SEISMIC INTENSITY DISTRIBUTION OF SHALLOW EARTHQUAKES DUE TO RUPTURE VELOCITIES AND FAULTING MODES. Acta Seismologica Sinica, 13(2): 190-201.
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[1] 国家地晨局,1979.中国地震等烈度腺图集,地震出版社.北京,1——107,
[2] 宇佐美翁夫,1987,新摄日本被害地震捻览.束京大学出版会.束京,1——434, [3] Campillo, M. and Bouchon, M., 1983. A theoretical study of the radiation from small strikeslip earthquakes at close distances. Buld. Seism. Soc. Amer,73, 83——96. [4] Cervenj., V., Popov, M. M.and Psencik, L, 1982. Computation of wave fields in iahomogeneous media——Gaussian beam approach. Geophyr. J. R. astr. Soc., 70, 109——128. [5] Trifunac, M, D. and Brady, A. G., 1975. On the correlation of seismic intensity scales with the peaks of recorded strong ground motion. Bull. Seism. Sac. Amer. 65, 139——162. [6] Koyama, J., 1985. Earthquake source time——function from coherent and incoherent rupture. Tectonophyrics, I18, 227——242. [7] 小山顺二,1987,短周期地震波。方位依存性.地震2,40,397——404, [8] Koyama, J. and Zheng, S. H., 1985. Excitation of short——period body——waves by great earthquakes. Phys. Earth Planet, later., 37, 108——123. [9] 小山顺二,1988,震度分布t断屠遐勤一加速度。方位依存性.地震,41,79——87, [10] 小山顺二、泉谷恭男,1988.最大加速度、1964年新渴地震乏1983年日本海中部地震.地震,41,1——8 [11] Boore, D. M., 1983. Stochastic simulation of high——frequency ground motions based on seismological models of the radiated Koyama, J. and Shimada. N spectra. Bull. Seism. Sac, Amer., 73, 1865——1894. [12] Physical basis of earthquake magnitudes: An extreme value of seismic amplitudes from incoherent fracture of random fault patches. Phyr. Earth Planet.Inter., 40, 301——308. [13] Gutenberg, B. and Richter, C. F., 1942. Earthquake magnitude, intensity, energy, and acceleraLion. Bull. Seism. Soc. Amen, 32, 163——191. [14] Hirasawa, T 1965. Source mechanism of the Niigata earthquake of June 16, 1964, as derived from body waves. J. Phys. Earth., 13, 35——66. [15] 茅野一郎 1973.近地地震。震源决定地震。地震研究所研究.束京大学,12,83——98, [16] Kawasumi, H. and Sato, Y., 1968. Intensity of Niigata earthquake as determined from questionnaires. General Rep. Niigata Earthq. 1964. Tokyo Elec. Eng. Coll., 175——179. [17] 河角店X1973.地震炎害,共立出版,束京.1——276. [18] 梅世蓉X1982, 1976年唐山地展,地震出版社,北京.1——459, [19] Butler, R., Stewart, G. S, and Kanamori, H., 1979. The July 27, 1976 Tangshan, China earthquake——A complex sequence of intraplate events. Bull. Seism. Soc. Amer. 69, 207——220. [20] Chen, P. and Nuttli, O. W., 1984. Estimates of magnitudes and short——period :wave attenuation of Chinese earthquakes from modified ,Mercalli intensity data. Bull. Seism. Soc. Amen, 74,957——9ti8. [21] ;,ato, T Kosuga, M Tanaka, K, and Sato, H., 1986. Aftershock distribution the 1983 Nihonkai——chubu (Japan Sea) earthquake determined from relocated hypocenters. J. Phys. Earth.34, 203——223. [22] 太田裕、镜味洋史、俊藤典俊、同田成幸、掘田淳、1984, 4, 2, 2, 1983年日本海中部地震,北北海道地域市时村震度稠查.1983年日本海中部地震稠查研究 176——179, [23] Hashida, T, and Shimazaki, K., 1987. Predicting JMA seismic intensities based on 3——D attenuanon structure and suface amplifying factor: The Tohoku district, Japan. J. Phys. Earrh., 35,367——379. [24] Cipar, J., 1979. Source processes of the Haicheng, China earthquake from observations of Ptnd S waves. Bull. Seism. Soc. Amen, 69, 1903——1916. [25] 蒋凡,1978.海城地震,地震出版社,北京.1——90, [26] Zhou, H., Allen, C. R. anti Kanamori, H., 19836, Rupture complexity of the 1970 Tonghai and 1973 Luhuo earthquakes, China, from P——wave inversion, and relationship to surface faultingBull. Seism. Sot. Amen, 73, 1585——1597. [27] Kanamori, H. and Anderson, D. L., 1975. Theoretical basis of some empirical relations in seisinology. Bull. Seirm. Sot. Amen, 65, 1073——1095. [28] Brune, J. N. and King, D. Y., 1967. Excitation of mantle Rayleigh waves of period 100 seconds as a function of magnitude. Bull. Seism. Soc. Amen, 57, 1355——1385. [29] Koyama, J., Takemura, M. and Suzuki, Z., 1982. A scaling model for quantification of rthquakes in anal near Japan. Tectonophysicr, 84, 3——16. [30] Koyama, J., 1987. Focal mechanism of tsunami and tsunamigenic earthquakes. Yroc. Intern.Tsunami Symp. 1987, in press, lUGG. [31] Aki, K., 1966. Generation and propagation of G waves from the Niigata earthquake of June 16, 1964. Bull. Earzhg. Res. Inst., Tokyo Ilniv., 44, 23——88. [32] 7hou, H., Liu, H. L. and Kanamori, H., 1983. Source process of large earthquakes along the Xianshuihe fault in Southwestern China. Bull. Seism. Sac. timer 73, 537——551. [33] Zheng, S., 1983. Seismic moment tensor inversion of earthqaukes in and near the Tibetan plateau.博士学位论文,束北大学理学部,1——187,
[1] 国家地晨局,1979.中国地震等烈度腺图集,地震出版社.北京,1——107,
[2] 宇佐美翁夫,1987,新摄日本被害地震捻览.束京大学出版会.束京,1——434, [3] Campillo, M. and Bouchon, M., 1983. A theoretical study of the radiation from small strikeslip earthquakes at close distances. Buld. Seism. Soc. Amer,73, 83——96. [4] Cervenj., V., Popov, M. M.and Psencik, L, 1982. Computation of wave fields in iahomogeneous media——Gaussian beam approach. Geophyr. J. R. astr. Soc., 70, 109——128. [5] Trifunac, M, D. and Brady, A. G., 1975. On the correlation of seismic intensity scales with the peaks of recorded strong ground motion. Bull. Seism. Sac. Amer. 65, 139——162. [6] Koyama, J., 1985. Earthquake source time——function from coherent and incoherent rupture. Tectonophyrics, I18, 227——242. [7] 小山顺二,1987,短周期地震波。方位依存性.地震2,40,397——404, [8] Koyama, J. and Zheng, S. H., 1985. Excitation of short——period body——waves by great earthquakes. Phys. Earth Planet, later., 37, 108——123. [9] 小山顺二,1988,震度分布t断屠遐勤一加速度。方位依存性.地震,41,79——87, [10] 小山顺二、泉谷恭男,1988.最大加速度、1964年新渴地震乏1983年日本海中部地震.地震,41,1——8 [11] Boore, D. M., 1983. Stochastic simulation of high——frequency ground motions based on seismological models of the radiated Koyama, J. and Shimada. N spectra. Bull. Seism. Sac, Amer., 73, 1865——1894. [12] Physical basis of earthquake magnitudes: An extreme value of seismic amplitudes from incoherent fracture of random fault patches. Phyr. Earth Planet.Inter., 40, 301——308. [13] Gutenberg, B. and Richter, C. F., 1942. Earthquake magnitude, intensity, energy, and acceleraLion. Bull. Seism. Soc. Amen, 32, 163——191. [14] Hirasawa, T 1965. Source mechanism of the Niigata earthquake of June 16, 1964, as derived from body waves. J. Phys. Earth., 13, 35——66. [15] 茅野一郎 1973.近地地震。震源决定地震。地震研究所研究.束京大学,12,83——98, [16] Kawasumi, H. and Sato, Y., 1968. Intensity of Niigata earthquake as determined from questionnaires. General Rep. Niigata Earthq. 1964. Tokyo Elec. Eng. Coll., 175——179. [17] 河角店X1973.地震炎害,共立出版,束京.1——276. [18] 梅世蓉X1982, 1976年唐山地展,地震出版社,北京.1——459, [19] Butler, R., Stewart, G. S, and Kanamori, H., 1979. The July 27, 1976 Tangshan, China earthquake——A complex sequence of intraplate events. Bull. Seism. Soc. Amer. 69, 207——220. [20] Chen, P. and Nuttli, O. W., 1984. Estimates of magnitudes and short——period :wave attenuation of Chinese earthquakes from modified ,Mercalli intensity data. Bull. Seism. Soc. Amen, 74,957——9ti8. [21] ;,ato, T Kosuga, M Tanaka, K, and Sato, H., 1986. Aftershock distribution the 1983 Nihonkai——chubu (Japan Sea) earthquake determined from relocated hypocenters. J. Phys. Earth.34, 203——223. [22] 太田裕、镜味洋史、俊藤典俊、同田成幸、掘田淳、1984, 4, 2, 2, 1983年日本海中部地震,北北海道地域市时村震度稠查.1983年日本海中部地震稠查研究 176——179, [23] Hashida, T, and Shimazaki, K., 1987. Predicting JMA seismic intensities based on 3——D attenuanon structure and suface amplifying factor: The Tohoku district, Japan. J. Phys. Earrh., 35,367——379. [24] Cipar, J., 1979. Source processes of the Haicheng, China earthquake from observations of Ptnd S waves. Bull. Seism. Soc. Amen, 69, 1903——1916. [25] 蒋凡,1978.海城地震,地震出版社,北京.1——90, [26] Zhou, H., Allen, C. R. anti Kanamori, H., 19836, Rupture complexity of the 1970 Tonghai and 1973 Luhuo earthquakes, China, from P——wave inversion, and relationship to surface faultingBull. Seism. Sot. Amen, 73, 1585——1597. [27] Kanamori, H. and Anderson, D. L., 1975. Theoretical basis of some empirical relations in seisinology. Bull. Seirm. Sot. Amen, 65, 1073——1095. [28] Brune, J. N. and King, D. Y., 1967. Excitation of mantle Rayleigh waves of period 100 seconds as a function of magnitude. Bull. Seism. Soc. Amen, 57, 1355——1385. [29] Koyama, J., Takemura, M. and Suzuki, Z., 1982. A scaling model for quantification of rthquakes in anal near Japan. Tectonophysicr, 84, 3——16. [30] Koyama, J., 1987. Focal mechanism of tsunami and tsunamigenic earthquakes. Yroc. Intern.Tsunami Symp. 1987, in press, lUGG. [31] Aki, K., 1966. Generation and propagation of G waves from the Niigata earthquake of June 16, 1964. Bull. Earzhg. Res. Inst., Tokyo Ilniv., 44, 23——88. [32] 7hou, H., Liu, H. L. and Kanamori, H., 1983. Source process of large earthquakes along the Xianshuihe fault in Southwestern China. Bull. Seism. Sac. timer 73, 537——551. [33] Zheng, S., 1983. Seismic moment tensor inversion of earthqaukes in and near the Tibetan plateau.博士学位论文,束北大学理学部,1——187, |
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| Lu ZAOXUNup, Liu GUODONGup2, WEI MENGHUAup2, MENG PUZAIup, ZHAO JUNMENGuploalucash. 1990: LATERAL INHOMOGENEITY OF CRUST AND UPPER MANT-LE IN SOUTH LIAONING, CHINA AND ITS RELATIONSHIP WITH THE M 7.3 HAICHENG EARTHQUAKE. Acta Seismologica Sinica, 12(4): 367-378. | |
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