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Ground motion and rupture process of the 2004 Mid Niigata Prefecture earthquake obtained from strong motion data of K-NET and KiK-net
Earth, Planets and Space volume 57, pages527–532(2005)
The 2004 Mid Niigata Prefecture earthquake (37.289°N, 138.870°E, 13.1 km, MJMA 6.8; JMA), also known as the 2004 Niigata Prefecture Chuetsu earthquake, was a thrust type earthquake that occurred on October 23, 2004 at 17:56 (JST). Strong ground motions of PGA 800-1700 cm/s2 and PGV 60-130 cm/s were observed at stations located immediately above the source region. We deduced the rupture process of this earthquake with a multi-time-window linear waveform inversion procedure. We used near-fault strong ground motion data observed at nine K-NET and KiK-net stations within 50 km from the epicenter. In order to obtain appropriate Green’s functions for the waveform inversion, we constructed two velocity structure models for stations on the hanging wall and one structure model for stations on the footwall. The estimated total slip distribution contains three asperities: (a) around the hypocenter, (b) in the upper-middle section of the fault plane, and (c) southwest of the hypocenter. The maximum slip is 3.8 m at the hypocenter and the total seismic moment is 1.2 × 1019 Nm, which corresponds to Mw=6.7. The moment rate functions in asperities (a) and (c) have a short rise time, while those in asperity (b) have a longer rise time.
Akaike, H., Likelihood and the Bayes procedure, in Bayesian Statics, University Press, Valencia, Spain, 1980.
Aoi, S., K. Obara, S. Hori, K. Kasahara, and Y. Okada, New Strong-Motion Observation Network: KiK-net, EOS Trans. Am. Geophys. Union, p. 329, 2000.
Aoi, S., N. Morikawa, R. Honda, H. Sekiguchi, T. Kunugi, and H. Fujiwara, Large ground-motion observed during 2004 Niigata-ken Chuetsu Earthquake, Report on the Damage Investigation of the 2004 Mid Niigata Prefecture Earthquake, 10–17. Japanese Geotechnical Society, 2005 (in Japanese).
Bouchon, M., A simple method to calculate Green’s function for elastic layered media, Bull. Seis. Soc. Am., 71, 959–971, 1981.
Fukuyama, E., M. Ishida, S. Hori, S. Sekiguchi, and S. Watada, Broadband seismic observation conducted under the FREESIA Project, Rep. Nat’l. Res. Inst. Earth Sci. Disas. Prev., 57, 23–31, 1996.
Hartzell, S. H. and T. Heaton, Inversion of strong ground motion and teleseismic waveform data for the fault rupture history of the 1979 Imperial Valley, California, earthquake, Bull. Seis. Soc. Am., 73, 1553–1583, 1983.
Kamae, K., T. Ikeda, and S. Miwa, Source model composed of asperities for the 2004 Mid Niigata Prefecture, Japan, earthquake (MJMA = 6.8) by the forward modeling using the empirical Green’s function method, Earth Planets Space, 57, this issue, 533–538, 2005.
Kennett, B. L. N., Seismic Wave Propagation in Stratified Media, Cambridge University Press, Cambridge, 1983.
Kinoshita, S., Kyoshin net (K-NET), Seism. Res. Lett., 69, 309–332, 1998.
Kobayashi, I., M. Takeishi, T. Yoshioka, and M. Shimazu, Geology of the Nagaoka district with geological sheet map at 1:50,000. Geological Survey of Japan, 132 pp., 1991 (in Japanese with English abstract).
Lawson, C. and R. Hanson, Solving Least Squares Problems, Prentice-Hall, Inc., New Jersey, 1974.
Ministry of Economy, Trade and Industry, Report on Fundamental Exploration for Oil and Gas Resources in Japan, Fundamental Exploration Test Well “OGUNI”, p. 44, Japan Oil National Corporation, 2001.
Obara, K., Hi-net: High sensitivity seismograph network, Japan, Lecture Notes in Earth Sciences, 98, 79–87, 2002.
Sekiguchi, H., K. Irikura, and T. Iwata, Source inversion for estimating continuous slip distribution on the fault—Introduction of Green’s functions convolved with a correction function to give moving dislocation effects in subfaults, Geophys. J. Int., 150, 377–391, 2002.
Shiomi, K., K. Obara, S. Aoi, and K. Kasahara, Estimation on the azimuth of the Hi-net and KiK-net borehole seismometers, ZISIN, 56(1), 99–110, 2003 (in Japanese with English abstract and figure captions).
Si, H. and S. Midorikawa, New attenuation relationships for peak ground acceleration and velocity considering effect of fault type and site condition, J. Struct. Constr. Eng., 523, 63–70, 1999 (in Japanese with English abstract and figure captions).
Ukawa, M., M. Ishida, S. Matsumura, and K. Kasahara, Hypocenter determination method of the Kanto-Tokai observational network for mi-croearthquakes, Rep. Nat’l. Res. Inst. Earth Sci. Disas. Prev., 53, 1–88, 1984.
Wessel, P. and W. Smith, New version of the generic mapping tools, EOS Trans. Am. Geophys. Union, 76, 1995.
Yamanaka, H., K. Motoki, S. Fukumoto, H. Takahashi, N. Yamada, and K. Asano, Estimation of local site effects in Ojiya city using aftershock records of the 2004 Mid Niigata Prefecture earthquake and microtremors, Earth Planets Space, 57, this issue, 539–544, 2005.
Yanagisawa, Y., I. Kobayashi, K. Takeuchi, M. Takeishi, K. Kayahara, and T. Kato, Geology of the Odiya district with geological sheet map at 1:50,000, Geological Survey of Japan, 132 pp., 1986 (in Japanese with English abstract).
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Honda, R., Aoi, S., Morikawa, N. et al. Ground motion and rupture process of the 2004 Mid Niigata Prefecture earthquake obtained from strong motion data of K-NET and KiK-net. Earth Planet Sp 57, 527–532 (2005). https://doi.org/10.1186/BF03352587
- 2004 Mid Niigata Prefecture earthquake
- rupture process
- strong motion