Scaling Relations for Source Parameters Magnitude of Earthquakes in the Izu Peninsula Region, Japan
|
|
- Kristin Dalton
- 5 years ago
- Views:
Transcription
1 TOhoku Geophys. Journ. (Sci. Rep. TOhoku Univ., Ser. 5), Vol. 32, Nos. 3, 4, pp , Scaling Relations for Source Parameters Magnitude of Earthquakes in the zu Peninsula Region, Japan and MASAYUK TAKEMURA Kobori Research Complex, Kajima Corporation Akasaka , Minato-ku, Tokyo 107 TOMONOR KEURA Kajima nstitute of Construction Technology, Kajima Corporation Tobitakyu , Chofu-shi, Tokyo 182 RYOSUKE SATO Association for the Development of Earthquake Prediction Mitoshiro-cho 3, Chiyoda-ku, Tokyo 101 (Recieved November 18, 1989) Abstract : Relations among source parameters and magnitude are examined for the earthquakes in the zu peninsula region. Seismic moment M, and fault area S are newly evaluated from S-waves of strong motion records for the 1980 and 1983 earthquake swarm activities. t is found that Mo and S of the events satisfy the similarity relation in the Mo range from 1022 to 1026 dyne cm, which gives us the stress drops as being consistent with the world-wide average of shallow earthquakes. On the other hand, the relation between seismic moment Mo and JMA magnitude M is obtained as follows : log Mo=1.17M , which is not coincident with the average formula derived from the data for the events in and around Japan. JMA magnitude M of large events in the zu peninsula region shows larger value, when compared with M of the ordinary events with the same seismic moment. The same tendency is also found for inland shallow events in other regions. Judging from the results of the M,--S relation, it is difficult to conclude that the large value of M is due to anything unusual of source parameters. JMA magnitude M is usually determined from maximum amplitudes of seismic-waves at the period of several seconds observed in a local network. One of the possible reasons for the large value of M is in the difference of the excitation of the medium-period surface-waves. 1. ntroduction The zu peninsula, located about 100 km southwest of Tokyo, separates the two troughs of Sagami and Suruga, which are the tectonic boundaries between two plates of the Philippine Sea and the Honshu island (Sugimura, 1972 ; Nakamura, 1984). Moderate large earthquakes have occurred frequently in and around the zu peninsula since The hypocenters of these events are located at depths of 0 to 20 km in the shallower part of the Philippine Sea plate (shida, 1987). The major destructive events are the 1930
2 78 MASAYUK TAKEMURA, TOMONOR KEURA AND RYOSUKE SATO North-zu (M = 7.3), the 1974 zu-oki (M =6.9), the 1978 zu-oshima (M =7.0), and the 1980 zu-toho-oki (M =6.7) earthquakes. 11 earthquake swarm activities occurred east off the zu peninsula from 1978 to 1986 and the magnitude of the largest event of each swarm is 2.2 to 6.7 (shida, 1987). Many strong motion records have been obtained in the zu peninsula and in and around the Tokyo metoropolitan area of the recent large events and the earthquake swarm activities. Through the analyses of these records, it has been indicated that the short-period components of the seismic waves are small when compared with those of the events of the same magnitude occurring in other regions of Japan (e.g., Tanaka, 1979 : Nagahashi, 1983 ; Takemura and Ohta, 1983). According to these results, a question arises as to whether or not the scaling relations for source parameters arid magnitude are different in the zu peninsula region from other regions. Source parameters of the events in the zu peninsula region have been evaluated by using various kinds of observation records, and the relations among source parameters and magnitude have been investigated. Abe (1978), Shimazaki and Somerville (1979), and Takeo (1988), respectively, evaluated source parameters for the destructive large events from far-field long-period seismograms, near-field displacement type strongmotion records and the static displacement in the vicinity of the fault. Sasaki et al. (1981) analyzed accelerograms in near field for the aftershocks of the 1978 zu-oshima event, of which magnitude ranges from 1.2 to 2.5, and indicated that the stress drop ranges from 40 to 100 bar for most events. Tsujiura (1983) estimated source spectra for the foreshocks and aftershocks with magnitude of 3.2 to 5.8 of the 1978 zu-oshima event from the seismic-wave records at Dodaira which is about 100 km distance from the source region. t was concluded in spite of large scattering of data that the stress drop of foreshocks takes a low value when compared with that of the aftershocks. The stress drops of the aftershocks are almost consistent with the values estimated by Sasaki et al., (1981). Yoshida et al. (1988) analyzed P wave records obtained by the microearthquake observation and evaluated source parameters for events with magnitude from 1.6 to 4.1 of the 1985 earthquake swarm activity east off the zu peninsula. Some empirical relations among seismic moment, corner frequency of P-wave source spectrum, and magnitude were obtained for the micro-earthquakes. n the present study, we will newly evaluate source parameters for the 1980 and 1983 earthquake swarm activities and elucidate the scaling law of earthquakes in the zu peninsula region. For these purposes, strong motion records in near field are available. 2. Data and Method of Analysis Epicenters of analyzed earthquakes and locations of observation stations are shown in Fig. 1. Each station comprises a vertical array of accelerometers. The underground accelerometers in each station are located in a fairly hard stratum in the period of Miocene of the Tertiary, hence the amplification effects of the seismic waves due to the soft surface-layers are avoided. We analyzed the records by the underground accelerometers installed at GL-36 m in Shuzenji (SZJ) and at GL-38 m in Tateyama (TTY). Figure 2 shows the examples of accelerograms analyzed in this study. Cosine-type
3 SCALNG RELATONS FOR ZU PENNSULA EARTHQUAKES 79 okyo TTY Fig. 1 Locations of epicenters of analyzed events and of stations. the Shuzenji and Tateyama stations, respectively. 20.] SZJ NS.0 io 20 SZJ and TTY 5C indicate 60 h.0 B02 TTY NS MAX,3.379 Gai A -4.D 5EC/ 2^ 60 E NS Q to El NS SEC 813 SZJ MS ti 0 D A LSEC/ 40 Fig. 2 Examples of accelerograms for analyzed events io io to Fig. 3 Data window adopted for analysis of accelerograms. The length of the window to is 20 s for the 1980 main shock (M=-6.7) and 7 s for the other events.
4 80 MASAYUK TAKEMURA, TOMONOR KEURA AND RYOSUKE SATO tapered data-window in Fig. 3 is applied for the S-waves in the spectral analysis. The length of the window is to= 7s. Seismic-moment density M(f) is obtained from S-wave spectra to evaluate seismic moment Mo and fault area S for each event. The far-field spectral amplitude of S-waves Uo(f) in an infinite homogenious elastic medium can be written by the seismic-moment density M(f) as follows (e.g. Kanamori, 1972) : U0(f)=R00111(f)1 (47.60Vs3X) (1) where Roo is the point-source radiation coefficient, X the distance from the center of the fault to the observer, and Vs and p are S-wave velocity and density of the medium. Amplitude spectrum Us (f)obtained from the observed records is related to the spectral amplitude Uo(f) as follows : Us(f)---U0(.1)111(f)Hg(i) exp { 711X1 (Qs Vs )}, (2) where 1-1,(f) and Hg(f) are the absolute values of transfer functions due to instrumental response and ground response for incident seismic waves. The exponential term is for Table 1 Source Parameters of Analyzed Events No. Date and Time (JST) M X(km) (SZJ) Mo x 10" (dyne cm) S (km') JUN JUN JUN JUN JUN JUN JUN JUN JUN JUN JUN JUN JUL JUL JUL JUL JAN JAN JAN JAN JAN JAN t t t 73t t t t Average of the values at SZJ and at TTY
5 SCALNG RELATONS FOR ZU PENNSULA EARTHQUAKES 81 the effect of seismic energy attenuation along the propagation path from the source to the station. Qs is a quality factor for S-waves. Table 1 shows the list of analyzed earthquakes. M and X are earthquake magnitude in the JMA (Japan Meteorological Agency) scale and hypocentral distance for the SZJ station. While observed records at SZJ are analyzed for all the events, those at TTY are analyzed only for the Nos. 6, 271, 355, 360, 378, and 802 events, bacause observation records cannot be obtained for the other events at TTY. Results by moto et al. (1981) and moto (1984) indicated that almost all the analyzed events in this study show the strike slip on a vertical fault plane with the N-S strike, which is located in the shallower part of the crust. The TTY and SZJ stations are located respectively in the directions of west and east close to the focal regions. Therefore, SH-waves are dominant in NS-component at each station, hence it is pertinent that the radiation pattern coefficient R0 for the NS-components is taken as 1.0. The transfer function Hg(T) of ground response is assumed to be 2.0, in consideration of the SH-wave incidence to the ground with the outcrop of the hard stratum. This assumption is exactly valid at least in the frequency range lower than the natural frequency fo of the surface layers over the location of the underground accelerometers. ( a ) \ O2 i i \ /- \L' iliv\ 111\1 1, UL Z; V r; a~~ i 1,7, , " -- = \ ti-. - -,,, n C Li JAN (M=4. 5) SJ NS 1 4 _ X 106 0' 0 6 JAN. 20, 1983 (M=4.5) S/J NS ( -t a91 1! '3 2 5 (.) 2(1 FREQUENCY (Hz) Fig. 4 (a) An example of S-wave di: displacement-spectrum at SZJ corrected for the instrumental response 1W). (b) An example of S-wave displacement-spectrum at SZJ corrected for the instrumental response H1(f) and the effect of seismic energy attenuation along the propagation path. Quality factor Qs is assumed to be 200. Solid line indicates the envelope of the spectrum and fc is the corner frequency. :gl FREQUENCY (Hz)
6 82 MASAYUK TAKEMURA, TOMONOR KEURA AND RYOSUKE SATO Table 2. Source Parameters of Large Events Year M Mo (dyne cm) S (km2) References X x X X x 10" 1.3 X X x Abe (1978) Abe (1978) Abe (1978) Abe (1978) Abe (1978) Shimazaki and Somerville (1979) Fukuyama and rikura (1989) This study 10 ill 1 fc '\r\ o" 1, 4, aw >7.!t ar, J JUN (M =6 7) : C SZJ NS 11 1) 1_ riv, ( FREQUENCY (Hz) Fig. 5 S-wave spectrum at SZJ for the 1980 main shock (M=6.7) corrected for the instrumental reponse H1(f) and for the effect of seismic energy attenuation along the propagation path. Quality factor Q., is assumed to be 200. Solid line and f show the envelope of the spectrum and the corner frequency. The natural frequency of surface layers is about 3 Hz at both the SZJ and TTY stations. The accelerometers are force balance type with natural frequency of 450 Hz and damping constant of 0.7. The instrumental response can be approximately written as 1-11(f)---(2zf)Z in the frequency range from 0.1 to 50 Hz. Figure 4(a) shows an example of spectral amplitude of observed S-waves at SZJ for the Jan. 20, 1983 (No. 802) event. The spectrum is corrected for the instrumental response 111(f). The corner frequency can be identified at about 1.5 Hz. The spectrum is also corrected for inelastic attenuation using the Q, values of 200 for SZJ and of 500 for TTY. The Q, values are determined on the assumption that the high-frequency
7 SCALNG RELATONS FOR ZU PENNSULA EARTHQUAKES a (._., a., = >, 9:=, -_, o / //0 4./log mo 21( / i M Fig. 6 Relation between seismic moment Mo and JMA magnitude M for the events in the zu peninsula region. Solid circles indicate Mo's determined in this study and Open circles those obtained by other authors. The line (4) is the relation for the events in and around Japan by Sato (1979, 1989), and thick line (5) is that for the events in the zu peninsula region by the method of least squares. decay of source spectrum is proportional to f-2 (Aki, 1967). The determined values are consistent with (2,-value of the crust in northeastern Honshu, Japan by Umino and Hasegawa (1984). Figure 4(b) shows the corrected spectrum Us(f )/H(f)/exp { R-fX1 (Qs VS )}. The seismic moment Mo is evaluated from the spectral amplitude in the frequency range lower than the corner frequency ff. The numeral values of S-wave velocity and density are assumed to be Vs =3.8 km/ s and p =2.5 g/ cm. The source radius r is determined from fc on the basis of a circular crack model by Sato and Hirasawa (1973). On the assumption that the ratio of the rupture velocity Vr to the S- wave velocity V, is 0.8, the relation between r and fc may be written as follows : r =0.3 VS/ (3) The fault area S can be easily calculated from the source radius r. The seismic moment Mo and the fault area S are also shown for each event in Table 1. While the seismic moment Mo with a cross f in Table 1 is evaluated as the average of the values from observed spectra at SZJ and TTY, the fault area S is obtained from the corner frequency fc of the spectrum only at the SZJ station, in consideration of uncertainty of the attenuation correction for the distant station. 3. Results The magnitude range of the earthquakes listed in Table 1 is 3.1 to 4.9. To examine the relations among magnitude and source parameters, we also summarize in Table 2 as a reference the seismic moment M, and the fault area S of large events in the zu
8 84 MASAYUK TAKEMURA, TOMONOR KEURA AND RYOSUKE SATO o, 0 3 (6) 25 r r _ log S ( k rn2 ) Fig. 7 Relation between seismic moment Mo and fault area S for the events in the zu peninsula region. Solid and open circles indicate the data obtained in this study and by other authors, respectively. Solid line (6) is the relation determined for the events in and around Japan by Sato (1979, 1989) on the assumption of the similarity relations among source parameters. peninsula region by other authors. The seismic moment M. and the fault area S are redetermined by the method in the present study for the 1980 zu-toho-oki earthquake (M =6.7), which is the largest event in the 1980 earthquake swarm. Figure 5 shows the corrected spectrum at SZJ for the 1980 event. The data window of t0 = 20s is used for this event. The corrected spectrum shows that the co-2 fall-off in the frequency range higher than the corner frequency fc. M. and S obtained from the corrected spectrum are also listed in Table 2. The seismic moment M. obtained here is identical with the result by Fukuyama and rikura (1989), while the fault area S is a little smaller than the result as indicated by them. Fukuyama and rikura (1989) determined the fault area from the distribution of aftershocks of the 1980 event. Meanwhile, the fault area S in the present study is evaluated from the corner frequency of S-wave spectrum based on the circular crack model. t may be understood that the fault area estimated in this study corresponds to the area of large displacement on the fault plane (Fukuyama and rikura, 1989). To examine the relation between M. and S, we will adopt the value of fault area obtained from aftershock distribution, since the fault area for the other large earthquakes is estimated from aftershock region of each event. The relation between seismic moment M. and magnitude M is shown in Fig. 6. Sato
9 c SCALNG RELATONS FOR ZU PENNSULA EARTHQUAKES 85 (1979, 1989) determined the Mo-M relation from the data of earthquakes with M from 4 to 8 in and around Japan as follows : log Mo =1.5M (4) This relation is also shown in Fig. 6. We find that the relationship (4) cannot explain the data of large earthquakes in the zu peninsula region. The seismic moments of these events are meaningfully smaller than those calculated from M by the formula (4). A different relation is determined by the method of least squares as follows : proposed log Mo =1.17M (5) On the other hand, the relation between seismic moment Mo and fault area S by Sato (1979, 1989) explains the data of events in the zu peninsula region (Fig M (4) O 0/ 8 gc q) /(3... c.) 27 ca.) = 4,' 26 OPetle i./ iz.0 ch / /O0 41/ log m / o m (5) M Fig. 8 Relation between seismic moment Mo and JMA magnitude M for the events of the focal depth shallower than 80 km in and around Japan. The data are summarized by Sato (1989). Solid circles show the data for the inland events in the upper crust, and open circles those for the events in the subduction region along the Pacific coast of Japan and in the region along the eastern margin of the Japan sea. The relation (4) and (5) are explained in Fig. 6.
10 86 MASAYUK TAKEMURA, TOMONOR KEURA AND RYOSUKE SATO 7), though the Mo-S relation is obtained from the data of almost the same events for the determination of the Ma-M relation by Sato (1989). The relation by Sato (1979, 1989) is as follows : log Mo= 1.5 log S (6) This relation shows the condition of similarity of earthquake fault (Kanamori and Anderson, 1975). According to Aki (1967), the stress drop Zia on the fault plane is constant irrespectively of seismic moment under the similarity condition. Sato (1979, 1989) indicated that the equation (6) is derived under the assumption of lid= 50 bar. 4. Discussions Masuda (1988) indicated that the seismic moment Mo and corner frequency fc generally show the relation of Mocc fc-3 for the events of Mo from 1022 to 103 dyne cm occurring in various regions all over the world. The same result was obtained by Takemura and Koyama (1983) for the events of Mo from 1022 to 1029 dyne cm in the subduction region along the Japan trench. The relation between Mo and fc for the local earthquakes were examined by io (1986). According to the result by io (1986), the data of events of Mo from 10" to 1021 dyne cm does not support the relation of Moccf3 but the relation of M0ccfc4. Chouet et al. (1978) determined the scaling laws of earthquake source spectra in some regions, and indicated that the corner frequency fc is frequently constant irrespectively of seismic moment Mo for the events of M, smaller than 1022 dyne cm, while larger events show the relation of Mockfc-3. These results suggest that the earthquakes of seismic moment Mo larger than about 1022 dyne cm usually occur under the similarity condition of earthquake fault. The range of seismic moment of the events analyzed in the present study is about 1022 to 1026 dyne cm and the relation between seismic moment Mo and fault area S is explained by the formula (6), which shows the similarity condition of earthquake fault. The stress drop JO is estimated to be about 50 bar from the relation between Mo and S, which is consistent with the values for the 1978 zu-oshima event and its aftershocks by Sasaki et al. (1980), Shimazaki and Somerville (1979), and Tsujiura (1983). According to Geller (1976) and Kanamori and Anderson (1975), a good average of the stress drop is about 50 bar for shallow large events all over the world. it should be concluded from these facts that the earthquakes in the zu peninsula region have the same similarity condition of earthquake fault as ordinary shallow earthquakes. On the other hand, the data of seismic moment Mo and magnitude M for the events in the zu peninsula region cannot be explained by the relationship (4), which is obtained from the data of almost the same events used for determining the relationship (6). Figure 8 shows the comparison of the relationships (4) and (5) to the data of Mo and M for the earthquakes with focal depth shallower than 80 km in and around Japan, which were summarized by Sato (1989). Solid circles indicate the data of inland events occurring in the upper crust, which include the data of the events in the zu peninsula region. Their focal depths are shallower than 20 km. The earthquakes along the
11 SCALNG RELATONS FOR ZU PENNSULA EARTHQUAKES 87 eastern margin of the Japan sea are indicated by open circles. We can find that the solid circles are better explained by the formula (5). This indicates that the Mo-M relation obtained for the events in the zu peninsula region applies to the inland shallow earthquakes of other regions. Takemura and Ohta (1983) newly defined the magnitude scale Ma determined from peak accelerations of strong ground motions, and examined the difference between M and Ma for about 70 events in and around Japan from 1963 to The value of M. corresponds with the amplitude of source spectrum in the short period range, because peak acceleration is usually given by short period S-waves. Takemura and Ohta (1983) found four earthquakes showing significantly larger values of M than those expected from the average M-Ma relation. They all occurred inland, of which magnitude M is larger than 6.4 and the focal depth is shallower than 20 km. Three of them are the events in the zu peninsula region. These results suggest that inland shallow large events show larger M value when compared with the expected value not only from the seismic moment but also from the short-period amplitude of source spectrum. JMA magnitude is determined from the maximum amplitudes of seismic waves observed by the displacement-type seismographs with natural periods of about 5 s at many stations. The maximum amplitudes of the displacement records by JMA are usually given by surface-waves at the period of several seconds for shallow earthquakes (e.g. Mamula et al., 1985). Taking into account the shallow focal depth of the inland events, one of the possible reasons for the different relation between Mo and M is the large excitation of medium-period surface-waves near the source regions. The corrected S-wave spectrum in Fig. 5 of the 1980 zu-toho-oki event (M=6.7) can be explained by the co-square model (Aki, 1967) and does not show the anomalous large amplitude at the period of several seconds. This fact also supports the foregoing reason. 5. Conclusion The relations between seismic moment Mo and fault area S and between seismic moment Mo and JMA magnitude M are examined for the earthquakes in the zu peninsula region in the range of Mo from 1022 to 1026 dyne cm. be summarized as follows : The results obtained can (1) The seismic moment Mo and fault area S of these events are explained by the similarity relation by Sato (1979, 1989) as follows : log M0=1.5 log S (6) The stress drop Zic of these events is about 50 bar, which is consistent value of shallow earthquakes in various regions all over the world. (2) The M0-M relation of these events is obtained as follows : This is different with the average log Mo 1.17M (5) from the average formula derived from the data of events in and around Japan by Sato (1979, 1989). The JMA magnitude M of large events in the zu peninsula
12 88 MASAYUK TAKEMURA, TOMONOR KEURA AND RYOSUKE SATO region shows larger values, when compared with M of the ordinary events with the same seismic moment. These characteristics are also shown for inland shallow events in other regions. Meanwhile, JMA magnitude M shows the same tendency in its relation to peak accelerations of strong ground motions, which are usually given by short-period S-waves. Judging from the definition of the JMA magnitude M, one of the possible reasons for the large value of M is the difference of excitation of the medium-period surface-waves near the source regions. References Abe, K., 1978 : Dislocation, source dimensions and stresses associated with earthquakes in the zu Peninsula, Japan, J. Phys. Earth, 26, Aki, K., 1967 : Scaling law of seismic spectrum, J. Geophys. Res., 72, Chouet, B., K. Aki, and M. Tsujiura, 1978 : Regional variation of the scaling law of earthquake source spectra, Bull. Seism. Soc. Am., 68, Fukuyama, E, and K. rikura, 1989: Heterogeneity of the 1980 lzu-hanto-toho-oki earthquake rupture process, Geophys. J. nt., 99, Geller, R. J., 1976 : Scaling relations for earthquake source parameters and magnitude, Bull. Seism. Soc. Am., 66, io, Y., 1986: Scaling relation between earthquake size and duration of faulting for shallow earthquakes in seismic moment between 10" and 1025 dyne cm, J. Phys. Earth, 34, moto, M.,. Karakama, R.S. Matsu'ura, F. Yamazaki, and K. shibashi, 1981 : Focal mechanisms of the 1980 earthquake swarm off the east coast of the zu Peninsula, Japan, Zisin Ser., 34, (in Japanese with English abstract). moto, M., 1984 : Temporal change in the magnitude-frequency relation for the January 1983 zu earthquake swarm, Japan, Zisin Ser. 37, (in Japanese with English abstract) shida, M., 1987 : Recent activity in and around the zu peninsula, Proc. Earthq. Predict. Svmpo., (in Japanese with English abstract). Kanamori, H., 1972 : Mechanism of tsunami earthquakes, Phys. Earth Planet. nter., 5, Kanamori, H., and D.L. Anderson, 1975 : Theoretical basis of some empirical relations in seismology, Bull. Seism. Soc. Am., 65, Mamula, L., K. Kudo, and E. Shima, 1985 : Distribution of ground-motion amplification factors as a function of period (3-15 sec), in Japan, Bull. Earthq. Res. nst., 59, Masuda, T., 1988: Scaling law peculiar to micro-earthquakes, Mathematical Seismology (Suri- Jishin-gaku), 3, (in Japanese). Nakamura, K., 1984 : On a hypothesis of the Japan sea-fossa Magna plate boundary, The Earth Monthly, 6, (in Japanese). Nagahashi, S., 1983: A study on the effects of earthquake focal depth on the attenuation characteristics of ground motion amplitude against hypocentral distance, Summaries of Technical Papers of Alf, (in Japanese). Sasaki, S., H. Sawada, H. Yajima, and A. Sakurai, 1981 : On the characteristics of accelerograms recorded on bedrock near origins-part (2) Peak acceleration and source parameters, Rep. of Central Res. nst. of Electric Power nd., , 1-22 (in Japanese with English abstract). Sato, R., 1979: Theoretical basis on relationships between focal parameters and earthquake magnitude, J. Phys. Earth, 27, Sato, R., 1989 : Handbook of fault parameters for Japanese earthquakes, Kajima nstitute Publishing Co. LTD., (in Japanese). Sato, T., and T. Hirasawa, 1973 : Body wave spectra from propagating shear cracks, J. Phys. Earth, 21, Shimazaki, K. and P. Somerville, 1979 : Static and dynamic parameters of the zu-oshima-kinkai earthquake of January 14,1978, Bull. Seism. Soc. Am., 69, Sugimura, A., 1972 : Plate boundaries near Japan, KAGAKU, 42, (in Japanese). Takemura, M., and J. Koyama, 1983 : A scaling model of low-frequency earthquakes-relation of
13 SCALNG RELATONS FOR ZU PENNSULA EARTHQUAKES 89 source spectra between tsunami earthquakes and small low-frequency earthquakes, Zisin Ser. //, 36, (in Japanese). Takemura, M., and T. Ohta, 1983 : A new scale of earthquake magnitude based on observed acceleration amplitudes, Annual Rep. Kajima nst. Const. Tech., 31, (in Japanese with English abstract). Takeo, M., 1988: Rupture process of the 1980 zu-hanto-toho-oki earthquake deduced from strong motion seismograms, Bull. Seism. Soc. Am., 78, Tanaka, T., 1979 : A study on peak accelerations of recent destructive earthquakes, The 7 -th Sympo. on Ground Vibrations 3-8 (in Japanese). Tsujiura, M., 1983 : Waveform and spectral features of earthquake swarms and foreshoks in special reference to earthquake prediction, Bull. Earthq. Res. nst., 58, Umino, N., and A. Hasegawa, 1984 : Three-dimensional Qs structure in the northeastern Japan Arc, Zisin Ser., 37, (in Japanese with English abstract). Yoshida, M., M. Mizoue, H. Chiba, and H. Hagiwara, 1988 : P-wave source spectra and source parameters of small earthquakes near east coast of zu Peninsula, central Japan, Bull. Earthq. Res. nst., 63, (in Japanese with English abstract).
CHARACTERISTICS OF SOURCE SPECTRA OF SMALL AND LARGE INTERMEDIATE DEPTH EARTHQUAKES AROUND HOKKAIDO, JAPAN
13 th World Conference on Earthquake Engineering Vancouver, B.C., Canada August 1-6, 2004 Paper No. 1861 CHARACTERISTICS OF SOURCE SPECTRA OF SMALL AND LARGE INTERMEDIATE DEPTH EARTHQUAKES AROUND HOKKAIDO,
More informationA SEMI-EMPIRICAL METHOD USING A HYBRID OF STOCHASTIC AND DETERMINISTIC FAULT MODELS: SIMULATION OF STRONG GROUND MOTIONS DURING LARGE EARTHQUAKES
J. Phys. Earth, 36, 89-106, 1988 A SEMI-EMPIRICAL METHOD USING A HYBRID OF STOCHASTIC AND DETERMINISTIC FAULT MODELS: SIMULATION OF STRONG GROUND MOTIONS DURING LARGE EARTHQUAKES Masayuki TAKEMURA* and
More informationSource Characteristics of Large Outer Rise Earthquakes in the Pacific Plate
Source Characteristics of Large Outer Rise Earthquakes in the Pacific Plate T. Sasatani, N. Takai, M. Shigefuji, and Y. Miyahara Hokkaido University, Sapporo, Japan W. Kawabata Electric Power Development
More informationRECIPE FOR PREDICTING STRONG GROUND MOTIONS FROM FUTURE LARGE INTRASLAB EARTHQUAKES
RECIPE FOR PREDICTING STRONG GROUND MOTIONS FROM FUTURE LARGE INTRASLAB EARTHQUAKES T. Sasatani 1, S. Noguchi, T. Maeda 3, and N. Morikawa 4 1 Professor, Graduate School of Engineering, Hokkaido University,
More informationCoseismic slip distribution of the 1946 Nankai earthquake and aseismic slips caused by the earthquake
Earth Planets Space, 53, 235 241, 2001 Coseismic slip distribution of the 1946 Nankai earthquake and aseismic slips caused by the earthquake Yuichiro Tanioka 1 and Kenji Satake 2 1 Meteorological Research
More informationEffects of Surface Geology on Seismic Motion
4 th IASPEI / IAEE International Symposium: Effects of Surface Geology on Seismic Motion August 23 26, 2011 University of California Santa Barbara SCALING OF SHORT-PERIOD SPECTRAL LEVEL OF ACCELERATION
More informationRapid magnitude determination from peak amplitudes at local stations
Earth Planets Space, 65, 843 853, 2013 Rapid magnitude determination from peak amplitudes at local stations Akio Katsumata 1, Hiroshi Ueno 1, Shigeki Aoki 1, Yasuhiro Yoshida 2, and Sergio Barrientos 3
More informationUncertainties in a probabilistic model for seismic hazard analysis in Japan
Uncertainties in a probabilistic model for seismic hazard analysis in Japan T. Annaka* and H. Yashiro* * Tokyo Electric Power Services Co., Ltd., Japan ** The Tokio Marine and Fire Insurance Co., Ltd.,
More informationSecondary Love Waves Observed by a Strong-Motion Array In the Tokyo Lowlands, Japan
J. Phys. Earth, 40, 99-116, 1992 Secondary Love Waves Observed by a Strong-Motion Array In the Tokyo Lowlands, Japan Shigeo Kinoshita,1,* Hiroyuki Fujiwara,1 Tadashi Mikoshiba,1 and Tsutomu Hoshino2 National
More information(Somerville, et al., 1999) 2 (, 2001) Das and Kostrov (1986) (2002) Das and Kostrov (1986) (Fukushima and Tanaka, 1990) (, 1999) (2002) ( ) (1995
( ) 1995 ( ) (Somerville, et al., 1999) 2 (, 2001) (2001) Das and Kostrov (1986) (2002) Das and Kostrov (1986) GPS ) (Fukushima and Tanaka, 1990) (, 1999) (2002) ( ) (1995 1 (outer fault parameter) (inner
More informationMODELING OF HIGH-FREQUENCY WAVE RADIATION PROCESS ON THE FAULT PLANE FROM THE ENVELOPE FITTING OF ACCELERATION RECORDS
MODELING OF HIGH-FREQUENCY WAVE RADIATION PROCESS ON THE FAULT PLANE FROM THE ENVELOPE FITTING OF ACCELERATION RECORDS Yasumaro KAKEHI 1 SUMMARY High-frequency (higher than 1 Hz) wave radiation processes
More informationSource modeling of hypothetical Tokai-Tonankai-Nankai, Japan, earthquake and strong ground motion simulation using the empirical Green s functions
Source modeling of hypothetical Tokai-Tonankai-Nankai, Japan, earthquake and strong ground motion simulation using the empirical Green s functions Y. Ishii & K. Dan Ohsaki Research Institute, Inc., Tokyo
More informationSpatio-temporal variation in slip rate on the plate boundary off Sanriku, northeastern Japan, estimated from small repeating earthquakes
Spatio-temporal variation in slip rate on the plate boundary off Sanriku, northeastern Japan, estimated from small repeating earthquakes T. Matsuzawa, N. Uchida, T. Igarashi *, N. Umino, and A. Hasegawa
More informationAVERAGE AND VARIATION OF FOCAL MECHANISM AROUND TOHOKU SUBDUCTION ZONE
13 th World Conference on Earthquake Engineering Vancouver, B.C., Canada August 1-6, 24 Paper No. 414 AVERAGE AND VARIATION OF FOCAL MECHANISM AROUND TOHOKU SUBDUCTION ZONE Shunroku YAMAMOTO 1 Naohito
More informationScaling Relationship between the Number of Aftershocks and the Size of the Main
J. Phys. Earth, 38, 305-324, 1990 Scaling Relationship between the Number of Aftershocks and the Size of the Main Shock Yoshiko Yamanaka* and Kunihiko Shimazaki Earthquake Research Institute, The University
More informationFault Length and Direction of Rupture Propagation for the 1993 Kushiro-Oki Earthquake as Derived from Strong Motion Duration
Letter J. Phys. Earth, 41, 319-325, 1993 Fault Length and Direction of Rupture Propagation for the 1993 Kushiro-Oki Earthquake as Derived from Strong Motion Duration Yasuo Izutani Faculty of Engineering,
More informationSOURCE MODELING OF RECENT LARGE INLAND CRUSTAL EARTHQUAKES IN JAPAN AND SOURCE CHARACTERIZATION FOR STRONG MOTION PREDICTION
SOURCE MODELING OF RECENT LARGE INLAND CRUSTAL EARTHQUAKES IN JAPAN AND SOURCE CHARACTERIZATION FOR STRONG MOTION PREDICTION Kimiyuki Asano 1 and Tomotaka Iwata 2 1 Assistant Professor, Disaster Prevention
More informationAn intermediate deep earthquake rupturing on a dip-bending fault: Waveform analysis of the 2003 Miyagi-ken Oki earthquake
GEOPHYSICAL RESEARCH LETTERS, VOL. 31, L24619, doi:10.1029/2004gl021228, 2004 An intermediate deep earthquake rupturing on a dip-bending fault: Waveform analysis of the 2003 Miyagi-ken Oki earthquake Changjiang
More informationComplicated repeating earthquakes on the convergent plate boundary: Rupture processes of the 1978 and 2005 Miyagi-ken Oki earthquakes
Complicated repeating earthquakes on the convergent plate boundary: Rupture processes of the 1978 and 2005 Miyagi-ken Oki earthquakes Changjiang Wu 1 and Kazuki Koketsu Earthquake Research Institute, University
More informationTHREE-DIMENSIONAL FINITE DIFFERENCE SIMULATION OF LONG-PERIOD GROUND MOTION IN THE KANTO PLAIN, JAPAN
THREE-DIMENSIONAL FINITE DIFFERENCE SIMULATION OF LONG-PERIOD GROUND MOTION IN THE KANTO PLAIN, JAPAN Nobuyuki YAMADA 1 And Hiroaki YAMANAKA 2 SUMMARY This study tried to simulate the long-period earthquake
More informationSimulation of Strong Ground Motions for a Shallow Crustal Earthquake in Japan Based on the Pseudo Point-Source Model
6 th International Conference on Earthquake Geotechnical Engineering -4 November 25 Christchurch, New Zealand Simulation of Strong Ground Motions for a Shallow Crustal Earthquake in Japan Based on the
More informationCentroid moment-tensor analysis of the 2011 Tohoku earthquake. and its larger foreshocks and aftershocks
Earth Planets Space, 99, 1 8, 2011 Centroid moment-tensor analysis of the 2011 Tohoku earthquake and its larger foreshocks and aftershocks Meredith Nettles, Göran Ekström, and Howard C. Koss Lamont-Doherty
More informationA Prototype of Strong Ground Motion Prediction Procedure for Intraslab Earthquake based on the Characterized Source Model
A Prototype of Strong Ground Motion Prediction Procedure for Intraslab Earthquake based on the Characterized Source Model T. Iwata, K. Asano & H. Sekiguchi Disaster Prevention Research Institute, Kyoto
More informationVelocity Changes of Seismic Waves and Monitoring Stress in the Crust
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 12,**- pp.,+3,,0 + * +, +, Velocity Changes of Seismic Waves and Monitoring Stress in the Crust Muneyoshi Furumoto + *, Yoshihiro Hiramatsu + and Takashi Satoh,
More informationSource characterization of induced earthquakes by the 2011 off Tohoku, Japan, earthquake based on the strong motion simulations
Source characterization of induced earthquakes by the 2011 off Tohoku, Japan, earthquake based on the strong motion simulations K. Somei & K. Miyakoshi Geo-Reserch Institute, Osaka, Japan SUMMARY: A great
More informationRISKY HIGH-RISE BUILDINGS RESONATING WITH THE LONG-PERIOD STRONG GROUND MOTIONS IN THE OSAKA BASIN, JAPAN
RISKY HIGH-RISE BUILDINGS RESONATING WITH THE LONG-PERIOD STRONG GROUND MOTIONS IN THE OSAKA BASIN, JAPAN K. Miyakoshi 1 and M. Horike 2 ABSTRACT : 1 Earthquake Engineering Group, Geo-Research Institute,
More informationESTIMATION OF EFFECTIVE STRESS ON ASPERITIES IN INLAND EARTHQUAKES CAUSED BY LARGE STRIKE-SLIP FAULTS AND ITS APPLICATION TO STRONG MOTION SIMULATION
ESTIMATION OF EFFECTIVE STRESS ON ASPERITIES IN INLAND EARTHQUAKES CAUSED BY LARGE STRIKE-SLIP FAULTS AND ITS APPLICATION TO STRONG MOTION SIMULATION Kazuo DAN, Takayoshi MUTO, Jun'ichi MIYAKOSHI, and
More information4 Associate Professor, DPRI, Kyoto University, Uji, Japan
Proceedings of the International Symposium on Engineering Lessons Learned from the 2 Great East Japan Earthquake, March -4, 22, Tokyo, Japan STRONG MOTION ESTIMATION AT THE ELEVATED BRIDGES OF THE TOHOKU
More informationRE-EVALUATION OF NONLINEAR SITE RESPONSE DURING THE 1964 NIIGATA EARTHQUAKE USING THE STRONG MOTION RECORDS AT KAWAGISHI-CHO, NIIGATA CITY
969 RE-EVALUATION OF NONLINEAR SITE RESPONSE DURING THE 1964 NIIGATA EARTHQUAKE USING THE STRONG MOTION RECORDS AT KAWAGISHI-CHO, NIIGATA CITY Kazuyoshi KUDO 1, Tomiichi UETAKE 2 And Tatsuo KANNO 3 SUMMARY
More informationInversion Analysis of Historical Interplate Earthquakes Using Seismic Intensity Data
Inversion Analysis of Historical Interplate Earthquakes Using Seismic Intensity Data Katsuhisa Kanda and Masayuki Takemura Kobori Research Complex, Kajima Corporation, Tokyo 107-8502, Japan Summary An
More informationScattering and intrinsic attenuation structure in Central Anatolia, Turkey using BRTR (PS-43) array
Scattering and intrinsic attenuation structure in Central Anatolia, Turkey using BRTR (PS-43) array CTBT: Science & Technology 2011 Korhan Umut SEMIN Nurcan Meral OZEL B.U. Kandilli Observatory & Earthquake
More informationCoseismic slip distribution of the 2005 off Miyagi earthquake (M7.2) estimated by inversion of teleseismic and regional seismograms
Coseismic slip distribution of the 2005 off Miyagi earthquake (M7.2) estimated by inversion of teleseismic and regional seismograms Tadashi Yaginuma 1, Tomomi Okada 1, Yuji Yagi 2, Toru Matsuzawa 1, Norihito
More informationEARTHQUAKE SOURCE PARAMETERS OF MODERATELY EARTHQUAKE IN THE SOUTH EASTERN IRAN BASED ON TELESEISMIC AND REGIONAL DISTANCES
EARTHQUAKE SOURCE PARAMETERS OF MODERATELY EARTHQUAKE IN THE SOUTH EASTERN IRAN BASED ON TELESEISMIC AND REGIONAL DISTANCES M. Mostafazadeh 1 and S.Ashkpour Motlagh 2 1 Assistant Professor,Seismology Research
More informationGROUND MOTION SPECTRAL INTENSITY PREDICTION WITH STOCHASTIC GREEN S FUNCTION METHOD FOR HYPOTHETICAL GREAT EARTHQUAKES ALONG THE NANKAI TROUGH, JAPAN
GROUND MOTION SPECTRAL INTENSITY PREDICTION WITH STOCHASTIC GREEN S FUNCTION METHOD FOR HYPOTHETICAL GREAT EARTHQUAKES ALONG THE NANKAI TROUGH, JAPAN Masayuki YOSHIMI 1, Yasuto KUWAHARA 2, Masayuki YAMADA
More informationSPATIAL DISTRIBUTION OF STRONG GROUND MOTION CONSIDERING ASPERITY AND DIRECTIVITY OF FAULT
SPATIAL DISTRIBUTION OF STRONG GROUND MOTION CONSIDERING ASPERITY AND DIRECTIVITY OF FAULT Shunroku YAMAMOTO SUMMARY Waveform simulations of the 995 Hyogo-ken Nanbu earthquake were carried out to study
More informationPROBABILISTIC SEISMIC HAZARD MAPS AT GROUND SURFACE IN JAPAN BASED ON SITE EFFECTS ESTIMATED FROM OBSERVED STRONG-MOTION RECORDS
13 th World Conference on Earthquake Engineering Vancouver, B.C., Canada August 1-6, 2004 Paper No. 3488 PROBABILISTIC SEISMIC HAZARD MAPS AT GROUND SURFACE IN JAPAN BASED ON SITE EFFECTS ESTIMATED FROM
More informationStrong ground motions from the 2011 off-the Pacific-Coast-of-Tohoku, Japan (Mw=9.0) earthquake obtained from a dense nationwide seismic network
Landslides (2011) 8:333 338 DOI 10.1007/s10346-011-0279-3 Received: 10 June 2011 Accepted: 5 July 2011 Published online: 23 July 2011 The Author(s) 2011. This article is published with open access at Springerlink.com
More informationLONG-PERIOD SITE RESPONSE IN THE TOKYO METROPOLITAN AREA
Sixth International Conference on Urban Earthquake Engineering March 3-4, 2009, Tokyo Institute of Technology, Tokyo, Japan LONG-PERIOD SITE RESPONSE IN THE TOKYO METROPOLITAN AREA Kenichi Tsuda 1), Takashi
More informationMoment tensor inversion of near source seismograms
Moment tensor inversion of near source seismograms Yuji Yagi and Naoki Nishimura ABSTRACT We construct a program set for estimating moment tensor solution using near source seismograms. We take the effect
More informationFracture induced shear wave splitting in a source area of triggered seismicity by the Tohoku-oki earthquake in northeastern Japan.
Fracture induced shear wave splitting in a source area of triggered seismicity by the Tohoku-oki earthquake in northeastern Japan Masahiro Kosuga 1 1. Corresponding Author. Professor, Graduate School of
More informationNew Prediction Formula of Fourier Spectra Based on Separation Method of Source, Path, and Site Effects Applied to the Observed Data in Japan
New Prediction Formula of Fourier Spectra Based on Separation Method of Source, Path, and Site Effects Applied to the Observed Data in Japan Kenichi Nakano Graduate School of Engineering, Kyoto University,
More informationBROADBAND SOURCE MODEL AND STRONG MOTIONS
BROADBAND SOURCE MODEL AND STRONG MOTIONS OF THE 1855 ANSEI-EDO EARTHQUAKE ESTIMATED BY THE EMPIRICAL GREEN S FUNCTION METHOD Toshimi Satoh 1 1 Chief Researcher, Institute of Technology, Shimizu Corporation,
More informationPREDICTION OF STRONG MOTIONS FROM FUTURE EARTHQUAKES CAUSED BY ACTIVE FAULTS CASE OF THE OSAKA BASIN
PREDICTION OF STRONG MOTIONS FROM FUTURE EARTHQUAKES CAUSED BY ACTIVE FAULTS CASE OF THE OSAKA BASIN Kojiro IRIKURA 1 SUMMARY A methodology is proposed for estimating strong ground motions from scenario
More informationScaling of characterized slip models for plate-boundary earthquakes
LETTER Earth Planets Space, 6, 987 991, 28 Scaling of characterized slip models for plate-boundary earthquakes Satoko Murotani, Hiroe Miyake, and Kazuki Koketsu Earthquake Research Institute, University
More informationGEOPHYSICAL RESEARCH LETTERS, VOL. 31, L19604, doi: /2004gl020366, 2004
GEOPHYSICAL RESEARCH LETTERS, VOL. 31, L19604, doi:10.1029/2004gl020366, 2004 Characteristic seismic activity in the subducting plate boundary zone off Kamaishi, northeastern Japan, revealed by precise
More informationDYNAMIC DEFORMATION CHARACTERISTICS OF THE GROUND IDENTIFIED FROM SEISMIC OBSERVATIONS IN VERTICAL BOREHOLES
DYNAMIC DEFORMATION CHARACTERISTICS OF THE GROUND IDENTIFIED FROM SEISMIC OBSERVATIONS IN VERTICAL BOREHOLES Tetsushi KURITA 1, Hiroshi SATO 2 and Tomomi ADACHI 3 ABSTRACT Parameter identification analysis
More informationCentroid-moment-tensor analysis of the 2011 off the Pacific coast of Tohoku Earthquake and its larger foreshocks and aftershocks
LETTER Earth Planets Space, 63, 519 523, 2011 Centroid-moment-tensor analysis of the 2011 off the Pacific coast of Tohoku Earthquake and its larger foreshocks and aftershocks Meredith Nettles, Göran Ekström,
More informationEffect of the Emperor seamounts on trans-oceanic propagation of the 2006 Kuril Island earthquake tsunami
GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L02611, doi:10.1029/2007gl032129, 2008 Effect of the Emperor seamounts on trans-oceanic propagation of the 2006 Kuril Island earthquake tsunami S. Koshimura, 1 Y.
More informationThe late Prof. Tokuji Utsu: His career with Geophysics and Seismology
The late Prof. Tokuji Utsu: His career with Geophysics and Seismology R. S. Matsu ura 1 1 Association for the Development of Earthquake Prediction, 1-5-18, Sarugaku-cho, Chiyoda-ku, Tokyo 101-0064, Japan
More informationMechanics of Earthquakes and Faulting
Mechanics of Earthquakes and Faulting Lecture 20, 30 Nov. 2017 www.geosc.psu.edu/courses/geosc508 Seismic Spectra & Earthquake Scaling laws. Seismic Spectra & Earthquake Scaling laws. Aki, Scaling law
More informationEffects of subsurface structures of source regions on long period ground motions observed in the Tokyo Bay area, Japan
Uetake Earth, Planets and Space (27) 69:7 DOI.86/s4623-7-6-x LETTER Open Access Effects of subsurface structures of source regions on long period ground motions observed in the Tokyo Bay area, Japan Tomiichi
More informationSOURCE PROCESS OF THE 2003 PUERTO PLATA EARTHQUAKE USING TELESEISMIC DATA AND STRONG GROUND MOTION SIMULATION
Synopses of Master Papers Bulletin of IISEE, 47, 19-24, 2013 SOURCE PROCESS OF THE 2003 PUERTO PLATA EARTHQUAKE USING TELESEISMIC DATA AND STRONG GROUND MOTION SIMULATION Fabricio Moquete Everth* Supervisor:
More informationSource rupture process of the 2003 Tokachi-oki earthquake determined by joint inversion of teleseismic body wave and strong ground motion data
LETTER Earth Planets Space, 56, 311 316, 2004 Source rupture process of the 2003 Tokachi-oki earthquake determined by joint inversion of teleseismic body wave and strong ground motion data Yuji Yagi International
More informationEarthquake stress drop estimates: What are they telling us?
Earthquake stress drop estimates: What are they telling us? Peter Shearer IGPP/SIO/U.C. San Diego October 27, 2014 SCEC Community Stress Model Workshop Lots of data for big earthquakes (rupture dimensions,
More informationREPORT ON THE TOHOKU AREA PASIFIC OFFSHORE EARTHQUAKE
REPORT ON THE TOHOKU AREA PASIFIC OFFSHORE EARTHQUAKE GENERAL PERSPECTIVE The Highest Magnitude Ever Recorded The 2011 off the Pacific Coast of Tohoku Earthquake (hereafter, the 2011 Tohoku- Pacific Earthquake
More informationSOURCE MODELING OF SUBDUCTION-ZONE EARTHQUAKES AND LONG-PERIOD GROUND MOTION VALIDATION IN THE TOKYO METROPOLITAN AREA
SOURCE MODELING OF SUBDUCTION-ZONE EARTHQUAKES AND LONG-PERIOD GROUND MOTION VALIDATION IN THE TOKYO METROPOLITAN AREA ABSTRACT : Hiroe Miyake 1, Kazuki Koketsu 2, and Takashi Furumura 3,2 1 Assistant
More informationLong-period Ground Motion Characteristics of the Osaka Sedimentary Basin during the 2011 Great Tohoku Earthquake
Long-period Ground Motion Characteristics of the Osaka Sedimentary Basin during the 2011 Great Tohoku Earthquake K. Sato, K. Asano & T. Iwata Disaster Prevention Research Institute, Kyoto University, Japan
More informationUPPER MANTLE ATTENUATION STRUCTURE BENEATH THE EASTERN HOKKAIDO, JAPAN AND ITS EFFECTS ON STRONG GROUND MOTIONS
13 th World Conference on Earthquake Engineering Vancouver, B.C., Canada August 1-6, 2004 Paper No. 914 UPPER MANTLE ATTENUATION STRUCTURE BENEATH THE EASTERN HOKKAIDO, JAPAN AND ITS EFFECTS ON STRONG
More informationLong-period Ground Motion Simulation in Kinki Area. Nobuyuki YAMADA* and Tomotaka IWATA
Annuals of Disas. Prev. Res. Inst., Kyoto Univ., No. 47 C, 2004 Long-period Ground Motion Simulation in Kinki Area Nobuyuki YAMADA* and Tomotaka IWATA * COE Researcher, DPRI, Kyoto University Synopsis
More informationSeismic Activity and Crustal Deformation after the 2011 Off the Pacific Coast of Tohoku Earthquake
J-RAPID Symposium March 6-7, 2013 Seismic Activity and Crustal Deformation after the 2011 Off the Pacific Coast of Tohoku Earthquake Y. Honkura Tokyo Institute of Technology Japan Science and Technology
More informationThe Japanese University Joint Seismic Observations at the Niigaka-Kobe Tectonic Zone
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2*,**/ pp. +-- +.1 * The Japanese University Joint Seismic Observations at the Niigaka-Kobe Tectonic Zone The Japanese University Group of the Joint Seismic Observations
More informationNumerical simulation of seismic cycles at a subduction zone with a laboratory-derived friction law
Numerical simulation of seismic cycles at a subduction zone with a laboratory-derived friction law Naoyuki Kato (1), Kazuro Hirahara (2) and Mikio Iizuka (3) (1) Earthquake Research Institute, University
More informationNonlinear site response from the 2003 and 2005 Miyagi-Oki earthquakes
LETTER Earth Planets Space, 58, 1593 1597, 2006 Nonlinear site response from the 2003 and 2005 Miyagi-Oki earthquakes Kenichi Tsuda and Jamison Steidl Department of Earth Science and Institute for Crustal
More informationBROADBAND STRONG MOTION SIMULATION OF THE 2004 NIIGATA- KEN CHUETSU EARTHQUAKE: SOURCE AND SITE EFFECTS
Third International Symposium on the Effects of Surface Geology on Seismic Motion Grenoble, France, 30 August - 1 September 2006 Paper Number: 105 BROADBAND STRONG MOTION SIMULATION OF THE 2004 NIIGATA-
More informationIntrinsic and Scattering Seismic Attenuation in W. Greece
Pure appl. geophys. 153 (1998) 703 712 0033 4553/98/040703 10 $ 1.50+0.20/0 Intrinsic and Scattering Seismic Attenuation in W. Greece G-AKIS TSELENTIS 1 Abstract Intrinsic (Q 1 i ) and scattering (Q 1
More informationLETTER Earth Planets Space, 57, , 2005
LETTER Earth Planets Space, 57, 345 35, 25 Estimation of the source model for the foreshock of the 24 off the Kii peninsula earthquakes and strong ground motion simulation of the hypothetical Tonankai
More informationLETTER Earth Planets Space, 56, , 2004
LETTER Earth Planets Space, 56, 353 357, 2004 Deep seismic activities preceding the three large shallow earthquakes off south-east Hokkaido, Japan the 2003 Tokachi-oki earthquake, the 1993 Kushiro-oki
More informationGround Motion Validation of the +3,- Kanto Earthquake Using the New Geometry of the Philippine Sea Slab and Integrated -D Velocity-Structure Model
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2+,**0 pp.,01,1, Ground Motion Validation of the +3,- Kanto Earthquake Using the New Geometry of the Philippine Sea Slab and Integrated -D Velocity-Structure Model
More informationThe Focal Process of the Kita-Mino Earthquake 229
The Focal Process of the Kita-Mino Earthquake 229 field have been advanced. MARUYAMA (1963), HASKELL (1964, 1969) and SATO (1969) presented the mathematical formulae of the seismic waves due to a shear
More informationSlip distributions of the 1944 Tonankai and 1946 Nankai earthquakes including the horizontal movement effect on tsunami generation
Slip distributions of the 1944 Tonankai and 1946 Nankai earthquakes including the horizontal movement effect on tsunami generation Toshitaka Baba Research Program for Plate Dynamics, Institute for Frontier
More informationSTUDYING THE IMPORTANT PARAMETERS IN EARTHQUAKE SIMULATION BASED ON STOCHASTIC FINITE FAULT MODELING
STUDYING THE IMPORTANT PARAMETERS IN EARTHQUAKE SIMULATION BASED ON STOCHASTIC FINITE FAULT MODELING H. Moghaddam 1, N. Fanaie 2* and H. Hamzehloo 1 Professor, Dept. of civil Engineering, Sharif University
More informationDevelopment of a Predictive Simulation System for Crustal Activities in and around Japan - II
Development of a Predictive Simulation System for Crustal Activities in and around Japan - II Project Representative Mitsuhiro Matsu'ura Graduate School of Science, The University of Tokyo Authors Mitsuhiro
More informationThree Dimensional Simulations of Tsunami Generation and Propagation
Chapter 1 Earth Science Three Dimensional Simulations of Tsunami Generation and Propagation Project Representative Takashi Furumura Authors Tatsuhiko Saito Takashi Furumura Earthquake Research Institute,
More informationTokyo, Japan,
th International Conference on Structural Mechanics in Reactor Technology (SMiRT ) Espoo, Finland, August 9-4, 9 SMiRT -Division 4, Paper 389 Analysis of the strong motion records obtained from the 7 Niigataken
More informationFigure Locations of the CWB free-field strong motion stations, the epicenter, and the surface fault of the 1999 Chi-Chi, Taiwan earthquake.
2.2 Strong Ground Motion 2.2.1 Strong Ground Motion Network The world densest digital strong ground motion network of Taiwan with the station mesh of 3 km in the urban areas (Shin et al., 2) monitored
More informationEffects of Surface Geology on Seismic Motion
4 th IASPEI / IAEE International Symposium: Effects of Surface Geology on Seismic Motion August 23 26, 2011 University of California Santa Barbara TUNING THE DEEP VELOCITY STRUCTURE MODEL OF THE TOKYO
More informationNobuo Hurukawa 1 and Tomoya Harada 2,3. Earth Planets Space, 65, , 2013
Earth Planets Space, 65, 1441 1447, 2013 Fault plane of the 1964 Niigata earthquake, Japan, derived from relocation of the mainshock and aftershocks by using the modified joint hypocenter determination
More informationTsunami waveform analyses of the 2006 underthrust and 2007 outer-rise Kurile earthquakes
Author(s) 2008. This work is licensed under a Creative Commons License. Advances in Geosciences Tsunami waveform analyses of the 2006 underthrust and 2007 outer-rise Kurile earthquakes Y. Tanioka 1, Y.
More informationScenario Earthquake Shaking Maps in Japan
1 Scenario Earthquake Shaking Maps in Japan Nobuyuki Morikawa National Research Institute for Earth Science and Disaster Prevention (NIED), JAPAN Scenario Earthquake Shaking Maps (SESMs) The shaking maps
More informationMECHANISM OF THE 2011 TOHOKU-OKI EARTHQUAKE: INSIGHT FROM SEISMIC TOMOGRAPHY
Proceedings of the International Symposium on Engineering Lessons Learned from the 2011 Great East Japan Earthquake, March 1-4, 2012, Tokyo, Japan MECHANISM OF THE 2011 TOHOKU-OKI EARTHQUAKE: INSIGHT FROM
More informationSource Process and Constitutive Relations of the 2011 Tohoku Earthquake Inferred from Near-Field Strong-Motion Data
Source Process and Constitutive Relations of the 2011 Tohoku Earthquake Inferred from Near-Field Strong-Motion Data Kunikazu Yoshida, Anatoly Petukhin & Ken Miyakoshi Geo-Research Institute, Japan Koji
More informationHigh Acceleration Motions generated from the 2011 Pacific coast off Tohoku, Japan Earthquake
High Acceleration Motions generated from the 2011 Pacific coast off Tohoku, Japan Earthquake K. Irikura Disaster Prevention Research Center, Aichi Institute of Technology, Japan S. Kurahashi Disaster Prevention
More informationA METHOD FOR DETERMINING ASPERITY PARAMETERS PRODUCING SPECIFIC MAXIMUM GROUND MOTION
13 th World Conference on Earthquake Engineering Vancouver, B.C., Canada August 1-6, 24 Paper No. 395 A METHOD FOR DETERMINING ASPERITY PARAMETERS PRODUCING SPECIFIC MAXIMUM GROUND MOTION Masayuki YOSHIMI
More informationCrustal deformation by the Southeast-off Kii Peninsula Earthquake
Crustal deformation by the Southeast-off Kii Peninsula Earthquake 51 Crustal deformation by the Southeast-off Kii Peninsula Earthquake Tetsuro IMAKIIRE, Shinzaburo OZAWA, Hiroshi YARAI, Takuya NISHIMURA
More informationEarthquake Stress Drops in Southern California
Earthquake Stress Drops in Southern California Peter Shearer IGPP/SIO/U.C. San Diego September 11, 2009 Earthquake Research Institute Lots of data for big earthquakes (rupture dimensions, slip history,
More informationEFFECT OF RANDOM PARAMETERS IN SEMI-EMPIRICAL METHOD ON THE RESULTS OF GROUND MOTION PREDICTIONS
EFFECT OF RANDOM PARAMETERS IN SEMI-EMPIRICAL METHOD ON THE RESULTS OF GROUND MOTION PREDICTIONS J. Miyakoshi 1, K. Dan 1, A. Fukukita 1 and A. Okazaki 2 1 Shimizu Corporation, Tokyo, Japan 2 Kansai Electric
More informationSynthetic sensitivity analysis of high frequency radiation of 2011 Tohoku-Oki (M W 9.0) earthquake
Earthq Sci (214) 27(4):355 364 DOI 1.17/s11589-14-88-6 RESEARCH PAPER Synthetic sensitivity analysis of high frequency radiation of 211 Tohoku-Oki (M W 9.) earthquake Haoran Meng Yongshun John Chen Received:
More informationDi#erences in Earthquake Source and Ground Motion Characteristics between Surface and Buried Crustal Earthquakes
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2+,**0 pp.,/3,00 Di#erences in Earthquake Source and Ground Motion Characteristics between Surface and Buried Crustal Earthquakes Paul Somerville* and Arben Pitarka
More informationSTRONG GROUND MOTION ATTENUATION IN THE SEA OF JAPAN (OKHOTSK-AMUR PLATES BOUNDARY) REGION
13 th World Conference on Earthquake Engineering Vancouver, B.C., Canada August 1-6, 2004 Paper No. 197 STRONG GROUND MOTION ATTENUATION IN THE SEA OF JAPAN (OKHOTSK-AMUR PLATES BOUNDARY) REGION Laxman
More informationSource Parameters and Scaling Relation for Local Earthquakes in the Garhwal and Kumaun Himalaya, India
Cloud Publications International Journal of Advanced Seismology 2013, Volume 1, Issue 1, pp. 1-15, Article ID Sci-84 Research Article Open Access Source Parameters and Scaling Relation for Local Earthquakes
More informationFEASIBILITY STUDY ON EARTHQUAKE EARLY WARNING SYSTEM FOR THE CITY OF LIMA, PERU, USING A NEWLY DEPLOYED STRONG-MOTION NETWORK
FEASIBILITY STUDY ON EARTHQUAKE EARLY WARNING SYSTEM FOR THE CITY OF LIMA, PERU, USING A NEWLY DEPLOYED STRONG-MOTION NETWORK Cinthia CALDERON MEE1771 Supervisor: Takumi HAYASHIDA Toshiaki YOKOI ABSTRACT
More informationRELOCATION OF THE MACHAZE AND LACERDA EARTHQUAKES IN MOZAMBIQUE AND THE RUPTURE PROCESS OF THE 2006 Mw7.0 MACHAZE EARTHQUAKE
RELOCATION OF THE MACHAZE AND LACERDA EARTHQUAKES IN MOZAMBIQUE AND THE RUPTURE PROCESS OF THE 2006 Mw7.0 MACHAZE EARTHQUAKE Paulino C. FEITIO* Supervisors: Nobuo HURUKAWA** MEE07165 Toshiaki YOKOI** ABSTRACT
More informationA GLOBAL MODEL FOR AFTERSHOCK BEHAVIOUR
A GLOBAL MODEL FOR AFTERSHOCK BEHAVIOUR Annemarie CHRISTOPHERSEN 1 And Euan G C SMITH 2 SUMMARY This paper considers the distribution of aftershocks in space, abundance, magnitude and time. Investigations
More informationCONTROLLING FACTORS OF STRONG GROUND MOTION PREDICTION FOR SCENARIO EARTHQUAKES
13 th World Conference on Earthquake Engineering Vancouver, B.C., Canada August 1-6, 2004 Paper No. 2801 CONTROLLING FACTORS OF STRONG GROUND MOTION PREDICTION FOR SCENARIO EARTHQUAKES Hiroe MIYAKE 1,
More informationCHARACTERIZING EARTHQUAKE SLIP MODELS FOR THE PREDICTION OF STRONG GROUND MOTION
CHARACTERIZING EARTHQUAKE SLIP MODELS FOR THE PREDICTION OF STRONG GROUND MOTION P G SOMERVILLE 1, K IRIKURA, N ABRAHAMSON 3, S SAWADA 4, T KAGAWA 5 And Y TATSUMI 6 SUMMARY Over the past fifteen years,
More informationANALYTICAL STUDY ON RELIABILITY OF SEISMIC SITE-SPECIFIC CHARACTERISTICS ESTIMATED FROM MICROTREMOR MEASUREMENTS
ANALYTICAL STUDY ON RELIABILITY OF SEISMIC SITE-SPECIFIC CHARACTERISTICS ESTIMATED FROM MICROTREMOR MEASUREMENTS Boming ZHAO 1, Masanori HORIKE 2 And Yoshihiro TAKEUCHI 3 SUMMARY We have examined the site
More informationSource parameters of the 2011 Yellow Sea earthquake (M L 5.3): Different features from earthquakes on the Korean Peninsula
Earth lanets pace, 64, 379 388, 2012 ource parameters of the 2011 Yellow ea earthquake (M L 5.3): Different features from earthquakes on the Korean eninsula un-cheon ark, Min-Kyung Kong, Eun Hee ark, Won
More informationShort Note Fault Slip Velocities Inferred from the Spectra of Ground Motions
Bulletin of the Seismological Society of America, Vol. 99, No. 2A, pp. 876 883, April 2009, doi: 10.1785/0120080008 Short Note Fault Slip Velocities Inferred from the Spectra of Ground Motions by N. Ani
More informationREGIONAL CHARACTERISTICS OF STRESS FIELD AND ITS DYNAMICS IN AND AROUND THE NANKAI TROUGH, JAPAN
46 4 2003 7 CHINESE JOURNAL OF GEOPHYSICS Vol. 46, No. 4 July, 2003 1 1 2 3 1, 100037 2, 920-1192 3, 237-0061,,, : -. (10 22 ), (60 85km) ; (40 ), (160km)..,. GPS,, -,,.,,,.. 0001-5733(2003) 04-0488 -
More informationLong-period ground motion simulation in the Kinki area during the MJ 7.1 foreshock of the 2004 off the Kii peninsula earthquakes
LETTER Earth Planets Space, 57, 197 202, 2005 Long-period ground motion simulation in the Kinki area during the MJ 7.1 foreshock of the 2004 off the Kii peninsula earthquakes Nobuyuki Yamada and Tomotaka
More information