[PDF] Top 20 Fault model of the 2007 Noto Hanto earthquake estimated from PALSAR radar interferometry and GPS data
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Fault model of the 2007 Noto Hanto earthquake estimated from PALSAR radar interferometry and GPS data
... the fault plane are fixed to the value obtained in the previous subsection (Table ...strained from the used data ...the fault patches to be 0 km as our pre- ferred ...This model does not ... 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 fault, 18.6 km along the strike, is slightly shorter than that estimated by the inversion of the GPS data with fixed fault dip and strike based on the after- shock distribution ... See full document
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Postseismic displacements following the 2007 Noto peninsula earthquake detected by dense GPS observation
... northeastern Noto peninsula is hard to ex- plain with any mechanical ...source fault such as AKGM, SNDI, MNZN and ...ALOS/PALSAR data and showed a short wave length variation in fringes near ... See full document
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Fault model of the 2017 Jiuzhaigou Mw 6 5 earthquake estimated from coseismic deformation observed using Global Positioning System and Interferometric Synthetic Aperture Radar data
... Jiuzhaigou earthquake occurred in the northeast- ern part of the Tibetan ...which earthquake activity has been very strong during recent years (Deng et ...Jiuzhaigou earthquake occurred in the middle ... See full document
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Coseismic deformation of the 2007 Chuetsu oki earthquake derived from PALSAR/InSAR and its fault model
... Both fault planes are overlapped 5 km to avoid a marginal ...km fault segments, and the fault-slip vector at each segment was estimated by an inversion analysis based on the Okada model ... See full document
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Site amplification and strong ground motion of the 2007 Noto Hanto, Japan, earthquake estimated from aftershock observation
... assumed fault plane and the computed asperities are also shown. The fault plane’s location is based on fault models proposed from coastal deformation (Awata et ...2008), GPS and InSAR ... See full document
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Groundwater level changes related to the ground shaking of the Noto Hanto Earthquake in 2007
... extracted from the groundwater level data for 3 months before the Noto Hanto Earthquake using the BAYTAP-G program (Tamura et ...termined from these estimated tidal ... See full document
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Tsunami generated by the 2007 Noto Hanto earthquake
... the 2007 Noto Hanto earthquake are carried out for three models based on the coastal vertical movements, the GPS observations, and the strong-motion ...three fault models produce ... See full document
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Relation between similar aftershocks and ruptured asperity of a large inland earthquake: Example of the 2007 Noto Hanto earthquake
... the fault plane, while others do not. Nineteen groups are lying on the fault plane, and 11 groups are on the conju- gate ...source fault plane to investigate spatial relationship among the similar ... 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
... (JAXA, 2007; GSI, 2007; Fukushima et al., 2007) corresponds well to the KT ...inferred from SAR interferome- try indicates a large slip beneath the western sea area (GSI, ...constructed ... See full document
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Source model of the 2007 Noto Hanto earthquake (Mw 6 7) for estimating broad band strong ground motion
... motions from the mainshock are given as initial values from the empirical ...asperity model, the source area of the mainshock in (1) is replaced by that of the asperity, assuming that most of the ... 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
... by fault movement at the seismic source off the Noto ...tsunami from the earthquake would have required at least several tens of minutes to an hour to propagate around the Noto ... See full document
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Rupture process of the 2007 Noto Hanto earthquake: waveform inversion using empirical Green’s function
... mainshock fault plane of the 2007 Noto Hanto earthquake is relatively large and some of the stations which recorded the earthquake are lo- cated relatively close to the ... See full document
6
Observation of ground motions of aftershocks of the 2007 Noto Hanto earthquake in Monzenmachi, the Wajima city, for estimation of site amplification
... the northern mountains, while L2 and L3 were deployed on Quaternary layers. L3 is located on a small fan caused by another river, at a slightly higher elevation than that of L2. The former station is closest to the ... See full document
5
Three dimensional velocity structure in the source region of the Noto Hanto Earthquake in 2007 imaged by a dense seismic observation
... Fig. 1. Map of the relocated aftershock hypocenters determined by dou- ble-difference tomography, shown as circles scaled to earthquake mag- nitude and colored to depth. The red star denotes the epicenter of main- ... See full document
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Magnetotelluric observations around the focal region of the 2007 Noto Hanto Earthquake (Mj 6 9), Central Japan
... the 2007 Noto Hanto Earthquake is located above a conductive block (C1), and the aftershocks associated with the mainshock are also distributed along the top surface of this ...distance ... See full document
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Fault model of the 2005 Fukuoka ken Seiho oki earthquake estimated from coseismic deformation observed by GPS and InSAR
... fecture) earthquake occurred north of Fukuoka City, north- ern Kyushu, western Japan on March 20, 2005 ...Seiho-oki earthquake (hereafter Fukuoka earthquake) were ...the earthquake occurred ... 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
... strong-motion data from the 2007 Noto Hanto earthquake and separately estimate the spatio-temporal distributions of the seismic moment and effective stress on the ...motions ... See full document
6
Coulomb stresses imparted by the 25 March 2007 Mw=6 6 Noto Hanto, Japan, earthquake explain its ‘butterfly’ distribution of aftershocks and suggest a heightened seismic hazard
... an earthquake have been used to explain the spatial distri- bution of the subsequent aftershocks (Stein, 1999; Steacy et ...large earthquake trig- gering ...forecasting model of subsequent ... 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, as mentioned in the “Introduction” subsection, several slip models have reported a common feature of slip distribution: that is, a large coseismic slip area ... See full document
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