| Citation: |
Yong Sunup, Sihua Zhengup2, Shirong Meiup2p://dr=/. 1991: INVERSION OF SOURCE PARAMETERS AND ATTENUATION OF THE TANGSHAN AFTERSHOCKS. Acta Seismologica Sinica, 13(4): 422-429.
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[1] Aki, K.,1967. Scaling law of seismic spectrum. J. Geophys. Res., 72,1217——1231.
[2] Geller, R. J——1976. Scaling ralation for earthquake source parameters and magnitudes. Bull. Seis. Soc. Amer.66,1501——1523. [3] Papageorgiou, A. S. and Aki, K., 1985. Scaling law of farfield spectra based on observed parameters of the specific barrier model. PAGEOPN,123, 353——374. [4] Archulet, R. J——Cranswick, E., Mueller, C. and Spudish, P——1982. Source parameters of the 1980 Mammoth Lakes, California earthquake sequence. J. Geophys. Res., 87, 4595——4607. [5] Haar, L. C.,Fletcher, J. B. and Mueller, C. S——1984. The 1982 Eula, Arkansas, swarm and scaling of ground motion in the eastern United States. Bull. Seis. Soc. Amer. 74, 2463——2482. [6] Scherbaum. F. and Stoll, D., 1983 Source parameters and scaling laws of the 1978 Swabian Jura(Southwest Germany)aftershocks. Bull.&。.Soc. Amen,73, 1321——1343. [7] Johnson, L. R. and McEvilly, T. V., 1974. Nearfield observations and source parameters of central California earthquakes. Bull. Seis. Soc. Amer.,64, 1855——1886. [8] Dysart, P. S——Snoke, J. A. and Sacks, I. S., 1988. Source parameters and scaling relation for small earthquakes in the Matsushiro region, Southwest Honshu, Japan. Bull. Seis. Soc. Amer. 78, 571——589. [9] Hanks, T. C.,1982. fa Bull. Seis. Soc. Amen, 72, 1867——1879. [10] Das. S. and Aki, K.,1977. Fault plane with barriers:A versatile earthquake model. J. Geophys. Res.,82,5658——5670. [11] Papageorgion, A. S. and Aki, K., 1983. A specific barrier model for the quantitative description of inhomogeneous faulting and prediction of strong ground motion. I. Description of the model. Bull. Seis. Soc.Amer., 73, 693——722. [12] Papageorgion, A. S. and Aki, K., 1983b. A specific barrier model for the quantitative description of inhomogeneous faulting and prediction of strong ground motion. II.Application of the model. Bull. Seis. Soc. Amer.,73, 953——978 [13] Aki, K,1987. Magnitude——frequency relation for small earthquakes:A due to the origin of large earthquakes. J. Geophys. Res.,92, 1349——1355 [14] Papageorgion, A. S.,1988. On two characteristic frequencies of acceleration spectra: patch corner frequency and a Bull. Seis. Soc. Amer., 78, 509——529. [15] 范文、原秦喜、惠乃玲、李松林、石林可、张晓普,1987 滦县地区的近场观测.华北地震科学,5, 2, 40——50. [16] Brune, 3. N., 1970. Tectonic stress and spectra of seismic shear waves from earthquakes. J. Geophys. Res., 75,4997——5009. [17] Hanks, T. C. and Wyss, M., 1972 The use of body wave spectra in the determination of seismic source parameters. Bull. Seis. Soc. Amer.,62, 561——589. [18] Sato, T. and Hirasawa, T 1973.Body wave spectra from propagation shear cracks. J. Ps. Earth, 21,415——431. [19] Masuda, T.,1982. Scaling relations for source parameters of microearthquakes in the Northeastern part of Japan. Doctorial Thesis, Tohoku Univ., 67——70. [20] 大崎顺彦,1980.地震动的谱分析人门.地震出版社,北京180——186. [21] Garnet, M. and Trong, P. H., 1980. Some medium properties at Friuli ( Italy ) from amplitude spectrum analysis:a possible change in time or space. Tectonics, 68, 167——182. [22] Hasegawa, H. S.,1983. Lg spectra of Local earthquakes recorded by the eastern Canada telemetered network and spectral scaling. Bull. Seis. Soc. Amer.,73, 1041——1061. [23] Itovelli, A., Bonamassa, O.,Cocco, M——Bona, M. D. and Mazza, 5——1988. Scaling laws and spectral parameters of the ground motion in active extensional areas in Italy. Bull. Seis. Soc. Amer.78, 530——560 [24] Nuttli, O. W., 1983. Average seismicsource Amer,73, 519——535. [25] relations for mid——plate earthquakes. Bull. Seis. Soc. Joyner, W. B——1987. Strongmotion seismology. Rev. Geophys., 25. 1149——1160
[1] Aki, K.,1967. Scaling law of seismic spectrum. J. Geophys. Res., 72,1217——1231.
[2] Geller, R. J——1976. Scaling ralation for earthquake source parameters and magnitudes. Bull. Seis. Soc. Amer.66,1501——1523. [3] Papageorgiou, A. S. and Aki, K., 1985. Scaling law of farfield spectra based on observed parameters of the specific barrier model. PAGEOPN,123, 353——374. [4] Archulet, R. J——Cranswick, E., Mueller, C. and Spudish, P——1982. Source parameters of the 1980 Mammoth Lakes, California earthquake sequence. J. Geophys. Res., 87, 4595——4607. [5] Haar, L. C.,Fletcher, J. B. and Mueller, C. S——1984. The 1982 Eula, Arkansas, swarm and scaling of ground motion in the eastern United States. Bull. Seis. Soc. Amer. 74, 2463——2482. [6] Scherbaum. F. and Stoll, D., 1983 Source parameters and scaling laws of the 1978 Swabian Jura(Southwest Germany)aftershocks. Bull.&。.Soc. Amen,73, 1321——1343. [7] Johnson, L. R. and McEvilly, T. V., 1974. Nearfield observations and source parameters of central California earthquakes. Bull. Seis. Soc. Amer.,64, 1855——1886. [8] Dysart, P. S——Snoke, J. A. and Sacks, I. S., 1988. Source parameters and scaling relation for small earthquakes in the Matsushiro region, Southwest Honshu, Japan. Bull. Seis. Soc. Amer. 78, 571——589. [9] Hanks, T. C.,1982. fa Bull. Seis. Soc. Amen, 72, 1867——1879. [10] Das. S. and Aki, K.,1977. Fault plane with barriers:A versatile earthquake model. J. Geophys. Res.,82,5658——5670. [11] Papageorgion, A. S. and Aki, K., 1983. A specific barrier model for the quantitative description of inhomogeneous faulting and prediction of strong ground motion. I. Description of the model. Bull. Seis. Soc.Amer., 73, 693——722. [12] Papageorgion, A. S. and Aki, K., 1983b. A specific barrier model for the quantitative description of inhomogeneous faulting and prediction of strong ground motion. II.Application of the model. Bull. Seis. Soc. Amer.,73, 953——978 [13] Aki, K,1987. Magnitude——frequency relation for small earthquakes:A due to the origin of large earthquakes. J. Geophys. Res.,92, 1349——1355 [14] Papageorgion, A. S.,1988. On two characteristic frequencies of acceleration spectra: patch corner frequency and a Bull. Seis. Soc. Amer., 78, 509——529. [15] 范文、原秦喜、惠乃玲、李松林、石林可、张晓普,1987 滦县地区的近场观测.华北地震科学,5, 2, 40——50. [16] Brune, 3. N., 1970. Tectonic stress and spectra of seismic shear waves from earthquakes. J. Geophys. Res., 75,4997——5009. [17] Hanks, T. C. and Wyss, M., 1972 The use of body wave spectra in the determination of seismic source parameters. Bull. Seis. Soc. Amer.,62, 561——589. [18] Sato, T. and Hirasawa, T 1973.Body wave spectra from propagation shear cracks. J. Ps. Earth, 21,415——431. [19] Masuda, T.,1982. Scaling relations for source parameters of microearthquakes in the Northeastern part of Japan. Doctorial Thesis, Tohoku Univ., 67——70. [20] 大崎顺彦,1980.地震动的谱分析人门.地震出版社,北京180——186. [21] Garnet, M. and Trong, P. H., 1980. Some medium properties at Friuli ( Italy ) from amplitude spectrum analysis:a possible change in time or space. Tectonics, 68, 167——182. [22] Hasegawa, H. S.,1983. Lg spectra of Local earthquakes recorded by the eastern Canada telemetered network and spectral scaling. Bull. Seis. Soc. Amer.,73, 1041——1061. [23] Itovelli, A., Bonamassa, O.,Cocco, M——Bona, M. D. and Mazza, 5——1988. Scaling laws and spectral parameters of the ground motion in active extensional areas in Italy. Bull. Seis. Soc. Amer.78, 530——560 [24] Nuttli, O. W., 1983. Average seismicsource Amer,73, 519——535. [25] relations for mid——plate earthquakes. Bull. Seis. Soc. Joyner, W. B——1987. Strongmotion seismology. Rev. Geophys., 25. 1149——1160 |
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| Yu Tian Li Xiaojunupcom sh a. 2012: Inversion of strong motion data for source parametersof Wenchuan aftershocks, attenuation functionand average site effect. Acta Seismologica Sinica, 34(5): 621-632. | |
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| Peishan Chen, Tongxia Bai . 1991: QUANTIFICATION RELATIONS BETWEEN THE SOURCE PARAMETERS. Acta Seismologica Sinica, 13(4): 401-411. | |
| CHEN PEISHAN, CHEN HAITONG. 1989: SCALING LAW FROM TWO-DIMENSIONAL FAULTING MODEL. Acta Seismologica Sinica, 11(4): 337-350. | |
| 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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