Estimation of rupture propagation direction and strong motion generation area from azimuth and distance dependence of source amplitude spectra

Strong motion generation areas which reproduce ground motions in 0.2 to 10Hz were estimated using the empirical Green's function method. This strong motion generation area was somewhat smaller than the total rupture area, and coincident with the area of asperities derived from heterogeneous slip distributions estimated by waveform inversions using lower frequencies (<1Hz). We confirmed that the azimuth and distance dependence of observed source amplitude spectra in the near-source area, i.e. rupture directivity effects, were controlled by rupture propagation style and size of the strong motion generation area. We found that the source displacement spectra at stations in forward rupture propagation directions had higher corner frequencies and steeper high-frequency decays, compared with stations in sideways directions. Stations in backward directions had opposite tendencies. Different relationships between size and average corner frequencies of the strong motion generation area were proposed for unilateral and bilateral ruptures with radial propagation.

[1]  Walter H. F. Smith,et al.  New version of the generic mapping tools , 1995 .

[2]  Frank L. Vernon,et al.  Multitaper spectral analysis of high-frequency seismograms , 1987 .

[3]  Satoshi Ide Source process of the 1997 Yamaguchi, Japan, earthquake analyzed in different frequency bands , 1999 .

[4]  K. Irikura Prediction of strong acceleration motions using empirical Green's function , 1986 .

[5]  J. Mori Rupture directivity and slip distribution of the M 4.3 foreshock to the 1992 Joshua Tree earthquake, Southern California , 1996, Bulletin of the Seismological Society of America.

[6]  入倉 孝次郎,et al.  経験的グリーン関数法を用いた1997年3月26日 (MJMA6.5) 及び5月13日 (MJMA6.3) 鹿児島県北西部地震の強震動シミュレーションと震源モデル , 1999 .

[7]  N. Abrahamson,et al.  Characterizing Crustal Earthquake Slip Models for the Prediction of Strong Ground Motion , 1999 .

[8]  Kojiro Irikura,et al.  Source model of the 1995 Hyogo-Ken Nanbu earthquake and simulation of near-source ground motion , 1998, Bulletin of the Seismological Society of America.

[9]  Kojiro Irikura,et al.  Fault Geometry at the Rupture Termination of the 1995 Hyogo-ken Nanbu Earthquake , 2000 .

[10]  R. Madariaga Dynamics of an expanding circular fault , 1976, Bulletin of the Seismological Society of America.

[11]  Haruo Horikawa,et al.  Earthquake Doublet in Kagoshima, Japan: Rupture of Asperities in a Stress Shadow , 2001 .

[12]  N. Abrahamson,et al.  Modification of Empirical Strong Ground Motion Attenuation Relations to Include the Amplitude and Duration Effects of Rupture Directivity , 1997 .

[13]  Mizuho Ishida,et al.  Automated Seismic Moment Tensor Determination by Using On-line Broadband Seismic Waveforms , 1998 .

[14]  Charles S. Mueller,et al.  Source pulse enhancement by deconvolution of an empirical Green's function , 1985 .

[15]  D. Boore Stochastic simulation of high-frequency ground motions based on seismological models of the radiated spectra , 1983 .

[16]  Tomowo Hirasawa,et al.  Body wave spectra from propagating shear cracks. , 1973 .

[17]  J. Brune Tectonic stress and the spectra of seismic shear waves from earthquakes , 1970 .

[18]  W. B. Joyner,et al.  The effect of directivity on the stress parameter determined from ground motion observations , 1989 .

[19]  Shigeo Kinoshita,et al.  Kyoshin Net (K-NET) , 1998 .

[20]  W. B. Joyner,et al.  THE INFLUENCE OF RUPTURE INCOHERENCE ON SEISMIC DIRECTIVITY , 1978 .