[PDF] Top 20 Rupture process of the 2007 Noto Hanto earthquake: waveform inversion using empirical Green’s function
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Rupture process of the 2007 Noto Hanto earthquake: waveform inversion using empirical Green’s function
... the empirical Green’s function method, it is important to use small events that share the path and the site effects with the large ...the 2007 Noto Hanto earthquake is relatively ... See full document
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Rupture process of the 2007 Chuetsu oki, Niigata, Japan, earthquake—Waveform inversion using empirical Green’s functions—
... A waveform inversion was conducted to reveal the rupture process of the 2007 Chuetsu-oki, Niigata, Japan, earthquake using near-source strong ground motion ...as ... See full document
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Rupture process of the main shock of the 2016 Kumamoto earthquake with special reference to damaging ground motions: waveform inversion with empirical Green’s functions
... the rupture process of the main shock of the Kumamoto earthquake, particularly the generation of strong ground motions in the frequency range relevant to structural damage, was investigated based on ... See full document
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Rupture process by waveform inversion using simulated annealing and simulation of broadband ground motions
... of inversion is based on a review of previous studies. The idea of using observed records of a small event occur- ring near the source region of a large earthquake as an EGF was originally introduced ... See full document
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Rupture process during the 2007 Noto Hanto earthquake (MJMA 6 9) and strong motion simulation in the source region
... source inversion scheme com- posed of the empirical Green’s function method and sim- ulated annealing (Shiba and Irikura, 2005) to broadband strong-motion data from the 2007 Noto ... See full document
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Site amplification and strong ground motion of the 2007 Noto Hanto, Japan, earthquake estimated from aftershock observation
... the 2007 Noto Hanto earthquake, Monzen, Anamizu, and Wajima, are examined using aftershock records observed at eight temporary seismic stations installed just after the mainshock and at ... See full document
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Joint inversion of teleseismic, geodetic, and near field waveform datasets for rupture process of the 2015 Gorkha, Nepal, earthquake
... near-field waveform Green’s functions were computed by the methods of Kikuchi and Kanamori (2003), Zhu and Rivera (2002), and Kohketsu (1985), ...determined rupture front velocity was approximately 90 % of ... See full document
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Relationship between coseismic slip and static stress drop of similar aftershocks of the 2007 Noto Hanto earthquake
... the 2007 Noto Hanto earthquake, central Japan, and have examined the relationship between the coseismic slip of the mainshock and the static stress drop of the similar ...by using the ... See full document
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Source parameters of the 2007 Noto Hanto earthquake sequence derived from strong motion records at temporary and permanent stations
... shock) using those from an elemental small earthquake (aftershock) occurring close to the target earth- quake as Green’s ...The waveform synthesization is based on a rupture propa- gation: the ... See full document
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Automatic determination of source parameters of the 2007 Noto Hanto earthquake
... the rupture of several ...data using automatic P- and S-phase pickers, determine the focal mechanism, and identify the fault plane from two nodal ...the 2007 Noto Hanto ... See full document
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Radiated energy from the Noto Hanto, Japan, earthquake of March 25, 2007, and its aftershock
... source process of large and small ...seismogenic process in various tectonic ...of earthquake source when we predict strong ground motion due to future large earthquakes by the empirical ... See full document
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Source rupture processes of the foreshock and mainshock in the 2016 Kumamoto earthquake sequence estimated from the kinematic waveform inversion of strong motion data
... calculated using the discrete wavenumber method (Bouchon 1981) with the reflection and transmission matrix method (Kennett and Kerry ...smallest S-wave veloc- ity in this velocity structure model was 350 ... See full document
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Gravity anomalies and the geologic block structures in and around the aftershock area of the 2007 Noto Hanto Earthquake
... with the distribution of outcropping basement rocks. Figure 4 also shows a comparison between aftershock distributions provided by Japan Meteorological Agency (2007/03/25, 0:00–24:00) and the gravity anomalies. ... See full document
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Fault model of the 2007 Noto Hanto earthquake estimated from coseismic deformation obtained by the distribution of littoral organisms and GPS: Implication for neotectonics in the northwestern Noto Peninsula
... the Noto Peninsula during this rifting, those normal faults turned to reverse faults after the cease of the rifting due to the compressive stress associated with the forearc subduction (Katagawa et ...the ... See full document
11
Three dimensional velocity structure in the source region of the Noto Hanto Earthquake in 2007 imaged by a dense seismic observation
... west coast of the Noto Peninsula in Japan on March 25, 2007, inflicting serious damage in the surrounding areas. Aftershocks were distributed at the boundary between the area inland and the ocean to the west ... See full document
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Numerical simulation of the tsunami generated by the 2007 Noto Hanto Earthquake and implications for unusual tidal surges observed in Toyama Bay
... the earthquake (9:45 ...the earthquake (9:47 ...the earthquake (9:42 ...the earthquake, 9:46 a.m.) and the lowest level (7 min after the earthquake, 9:49 ...the earthquake (9:46 ... See full document
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Temporal variations of crustal structure in the source region of the 2007 Noto Hanto Earthquake, central Japan, with passive image interferometry
... 3.32 s–3.84 s, 4.31 s–4.77 s, 5.00 s–5.66 s, ...5.66 s–6.34 s, and 6.34 s–7.00 s, respectively ... See full document
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Fault model of the 2007 Noto Hanto earthquake estimated from PALSAR radar interferometry and GPS data
... As the earthquake occurred in a shallow crust, it caused ground surface displacements observable by geodetic tech- niques. The GPS network GEONET operated by the Ge- ographical Survey Institute (GSI) recorded up ... See full document
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Magnetotelluric observations around the focal region of the 2007 Noto Hanto Earthquake (Mj 6 9), Central Japan
... March 2007 near the west coast of the Noto Peninsula (Noto Hanto) which is located in the back arc area of Central Japan ...(NIED, 2007), this earthquake has a compressional axis ... See full document
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Does the 2007 Noto Hanto earthquake reveal a weakness in the Japanese national seismic hazard map that could be remedied with geological data?
... Abundant aftershocks have been recorded along the ENE-striking block-bounding faults, F14, F15, and F16 (Toda, 2008). Focal mechanisms of the moderate-sized aftershocks also suggest that the faulting mechanisms are ... See full document
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