[PDF] Top 20 Coseismic deformation due to the 2011 Tohoku oki earthquake: influence of 3 D elastic structure around Japan
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Coseismic deformation due to the 2011 Tohoku oki earthquake: influence of 3 D elastic structure around Japan
... of elastic heterogeneity on coseismic deformation associated with the 2011 Tohoku-oki earthquake, Japan, using a 3-D finite element model, ... See full document
15
Characteristics of postseismic deformation following the 2003 Tokachi oki earthquake and estimation of the viscoelastic structure in Hokkaido, northern Japan
... the 3-month dis- tribution and that the afterslip magnitude below the land is larger than that predicted from our logarithmic func- tion model throughout the analyzed ...the coseismic slip region, is a ... See full document
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Coulomb stress change for the normal fault aftershocks triggered near the Japan Trench by the 2011 Mw 9 0 Tohoku Oki earthquake
... In Figs. 4(a) and 4(b), we compare the Coulomb stress change calculated for the original plate boundary with that calculated for the elevated plate boundary. The Coulomb stress changes are those calculated for the slip ... See full document
5
Rheological profile across the NE Japan interplate megathrust in the source region of the 2011 Mw9 0 Tohoku oki earthquake
... brittle deformation and the dislocation creep flow laws for ductile deformation (Kohlstedt et ...NE Japan sub- duction zone by Shimamoto (1989, ...gigantic 2011 earthquake, was assigned ... See full document
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Monthly GRACE detection of coseismic gravity change associated with 2011 Tohoku Oki earthquake using northern gradient approach
... predicted coseismic gravity changes range from ...of coseismic gravity changes is associated with not only the uplift-subsidence deform- ation caused by elastic rebound but also the density de- ... See full document
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Surface rupture and characteristics of a fault associated with the 2011 and 2016 earthquakes in the southern Abukuma Mountains, northeastern Japan, triggered by the Tohoku Oki earthquake
... The 2011 Tohoku-Oki offshore subduction earthquake (M w ...in 2011 (M w ...northeastern Japan, where no active faults had been previously mapped by interpretation of aerial ...of ... See full document
23
Coseismic slip distribution of the 2011 off the Pacific coast of Tohoku Earthquake (M 9 0) estimated based on GPS data—Was the asperity in Miyagi oki ruptured?
... of Tohoku University spatially interpolates the nationwide GPS net- work, GEONET, which is managed by the Geospatial In- formation Authority of Japan ...the coseismic slip distribution especially ... See full document
6
Importance of rheological heterogeneity for interpreting viscoelastic relaxation caused by the 2011 Tohoku Oki earthquake
... postseismic deformation that exhibits short-term transi- ence followed by longer-term relaxation; therefore, this rheology is convenient for explaining the deformation rate change over ...instantaneous ... See full document
12
Estimation of three-dimensional crustal movements in the 2011 Tohoku-Oki, Japan, earthquake from TerraSAR-X intensity images
... also influence the layover shapes of the same building in the different ...observed around the Rifu GEONET station, which was the closest station to the focal ... See full document
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Coseismic Effects of the 2011 Magnitude 9 0 Tohoku Oki Earthquake Measured at Far East Russia Continental Coast by Gravity and GPS Methods
... hoku Earthquake of March 11, 2011, ...on Japan-Kamchatka-Alaska Subduc- tion Processes: Mitigating Risk through International Volcano, Earthquake, and Tsunami Science (JKASP- 2011), ... See full document
9
Strong localized asperity of the 2011 Tohoku Oki earthquake, Japan
... the Tohoku-Oki earthquake, and concluded that this region corresponds to the large co- seismic slip ...of Japan (GSI) performed a joint slip inversion of co-seismic GPS data from the Japanese ... See full document
6
Coseismic deformation of the 2007 Chuetsu oki earthquake derived from PALSAR/InSAR and its fault model
... of deformation along the anticline. Slight residuals of 2–3 cm were also distributed in the coastal area of Kashiwazaki on both de- scending and ascending ...is due to inadequate setting of the fault ... See full document
6
Detection of seismic events triggered by P waves from the 2011 Tohoku Oki earthquake
... currence remains unclear. The dynamic triggering of NVT by teleseismic waves provides a clue to understanding its mechanism because it is possible to directly investigate the stress/strain changes that excite NVT by ... See full document
7
A dynamic model of the frequency dependent rupture process of the 2011 Tohoku Oki earthquake
... We define the boundary between “deep” and “shallow” as a line striking 210 degrees at a distance of 0.5 degrees east from the epicenter. In each frame of the first 110 s of Meng et al. (2011)’s back-projection ... See full document
6
A comparison of different fractal analyses for VHF electromagnetic emissions and their self-organization for the off-sea Miyagi-prefecture earthquake
... But, 3 stations exhibited considerably differ- ent ...Fig. 3, we reject the f (α) curve ob- tained when the f (α) curve is not good enough to have the correlation coefficient less than ... See full document
9
Characteristics of deformation structure around the 2007 Niigata ken Chuetsu oki earthquake detected by multi channel seismic reflection imaging
... (MEXT, Japan), “Urgent study on the 2007 Niigata-ken Chuetsu-oki ...Chuetsu-oki earthquake were provided by Shinohara et ...from Japan Hydrographic Asso- ciation to produce the ... 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
... plotted coseismic displacement is the difference in the averages of daily solutions between March 10–19 and March ...Department, Japan Coast ...The coseismic displacement at these and the GEONET ... See full document
6
Crustal Deformation Studies using Synthetic Aperture Interferometry
... Gorkha earthquake by joint inversion of InSAR and GPS data ...The coseismic rupture of the Gorkha earthquake is dominated by thrust slip with a maximum value of ...maximum coseismic slip is ... See full document
10
Supercycle in great earthquake recurrence along the Japan Trench over the last 4000 years
... the Japan Trench, the mid-slope terrace (MST) is located at a depth of 4000–6000 ...the 2011 Tohoku, the 1896 Sanriku, the 1454 Kyotoku, and the 869 Jogan ...to earthquake shaking, the con- ... See full document
12
On the possibility of the 2011 Tohoku-oki earthquake reactivating Shinmoe-dake volcano, southwest Japan: insights from strain data measured in vaults
... the Tohoku-oki earthquake) acting on Shinmoe- dake were sufficiently large to trigger a volcanic eruption, and whether strain rates associated with magma accumula- tion show marked variations before ... See full document
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