[PDF] Top 20 Coseismic and postseismic crustal deformation after the Mw 8 Tokachi oki earthquake in Japan
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Coseismic and postseismic crustal deformation after the Mw 8 Tokachi oki earthquake in Japan
... the Tokachi area ruptured in the 1952 M w 8.2 earthquake, and the probability of the next earthquake within a 30 years period from 2003 has been estimated to be ∼60% (Earthquake Research Com- ... See full document
6
GPS observation of the first month of postseismic crustal deformation associated with the 2003 Tokachi oki earthquake (MJMA 8 0), off southeastern Hokkaido, Japan
... vertical deformation using a fault model shown in ...the coseismic fault predicts half to one-fifth subsidence of uplift caused by the deeper one ...the coseismic one occurred in the shallower part of ... See full document
6
Postseismic slip associated with the 2007 Chuetsu oki, Niigata, Japan, Earthquake (M 6 8 on 16 July 2007) as inferred from GPS data
... Postseismic crustal deformation associated with the 2007 Chuetsu-oki Earthquake, which occurred on 16 July 2007 with a magnitude of ...of Japan, near the coast of Mid-Niigata ... See full document
5
Coseismic deformation due to the 2007 Chuetsu oki earthquake (Mw= 6 8)
... the crustal structure than seismic data, incorporating a heterogeneous crustal structure could change the optimum source location by up to several kilometers ... See full document
6
Coseismic deformation due to the 2011 Tohoku oki earthquake: influence of 3 D elastic structure around Japan
... The layering and interface effects expectedly increase with an increase in the rigidity contrast. The displace- ment difference changes in magnitude, while the pattern remains the same (Fig. 5a–d). Changes in ... See full document
15
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 ... See full document
6
Coseismic and postseismic deformation associated with the 2016 Mw 7 8 Kaikoura earthquake, New Zealand: fault movement investigation and seismic hazard analysis
... that coseismic rupture not only occurred on shallow crustal faults but also at the Hikurangi subduction interface with small-scale thrust- ing-dominated movements (Hamling et ...Kaikoura earthquake ... See full document
14
Combined logarithmic and exponential function model for fitting postseismic GNSS time series after 2011 Tohoku Oki earthquake
... a postseismic deformation is commonly fitted by a logarithmic or exponential decay ...high-quality postseismic Global Navigation Satellite System (GNSS) time series of the 2011 Mw 9 Tohoku- ... See full document
12
Characteristics of postseismic deformation following the 2003 Tokachi oki earthquake and estimation of the viscoelastic structure in Hokkaido, northern Japan
... the coseismic slip area ...the coseismic slip area and its down-dip extension, ...the Tokachi Plain, which was not explained by the previous studies, but it is not considered to be totally artificial ... See full document
12
Crustal deformation and a preliminary fault model of the 2007 Chuetsu oki earthquake observed by GPS, InSAR, and leveling
... method. After trial and error modeling, we used four sets for fault dip as the initial parameters: one is that both segments of the faults dip northwest; another is that both segments of the faults dip southeast; ... See full document
6
Coseismic deformation of the 2007 Chuetsu oki earthquake derived from PALSAR/InSAR and its fault model
... The Japan Aerospace Explo- ration Agency (JAXA) carried out emergency observation by PALSAR (L-band synthetic aperture radar (SAR) sen- sor on the ALOS satellite) to gather information about the ground ... See full document
6
Coseismic and postseismic surface displacements of the 10 December 2003 (MW 6 5) Chengkung, eastern Taiwan, earthquake
... zontal displacements along the eastern margin of the Lon- gitudinal Valley which not surprisingly corresponds to the surface traces of the Chihshang fault and other segments of the LVF. To the east in the hanging-wall of ... See full document
17
Crustal Deformation Studies using Synthetic Aperture Interferometry
... Gorkha earthquake was possibly caused by the release of inter-seismic strain energy accumulated in the environs of mid-crustal ramp due to plate boundary ... See full document
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Source model composed of asperities for the 2003 Tokachi oki, Japan, earthquake (MJMA = 8 0) estimated by the empirical Green’s function method
... Irikura, K., Prediction of strong ground acceleration motions using empiri- cal Green’s function, Proc. 7th Japan Earthq. Eng. Symp., 151–156, 1986. Irikura, K., H. Miyake, T. Iwata, K. Kamae, H. Kawabe, and L. A. ... See full document
5
Changes in groundwater level associated with the 2003 Tokachi oki earthquake
... the earthquake, remarkable periodic oscillation in the groundwater levels started and continued for about one and three days in DT1 and DT2, ...the earthquake. The total increases until the ... See full document
6
Re estimation of tsunami source of the 1952 Tokachi oki earthquake
... 2003 Tokachi-oki earthquake tsunami (20 for deep ocean and 4 around tide gauge stations), but much smaller than 60 (about 1850 m) used by Hirata et ... See full document
8
Spatial distribution for moment tensor solutions of the 2003 Tokachi oki earthquake (MJMA = 8 0) and aftershocks
... The Pacific plate, overridden by the North American Plate, subducts obliquely at the Kuril trench situated to the south- east of Hokkaido at a rate of about 90 mm/year (Heki, 1989) (Fig. 1(a)). Nakanishi et al. (2001) ... See full document
6
Aseismic Deformation in Subduction Megathrusts: Central Andes and North-East Japan
... future earthquake is not well ...2011 earthquake potentially bringing this region closer to ...large earthquake in this ...the earthquake – actual slip amplitudes maybe larger if they occur ... 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
... strongest earthquake was the M8 Wudu earthquake that occurred in 1879 75 km east of the Jiuzhaigou ...strong earthquake was the Songpan earthquake sequence that occurred on the Huya Fault in ... See full document
12
Tsunami run up heights of the 2003 Tokachi oki earthquake
... The tsunami assessment was conducted immediately af- ter the earthquake. The survey along the southern coast of Hokkaido and the eastern coast of Tohoku was almost com- pleted by 29th of September, three days ... See full document
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