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[PDF] Top 20 Three dimensional S wave attenuation structure in and around source area of the 2018 Hokkaido Eastern Iburi Earthquake, Japan

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Three dimensional S wave attenuation structure in and around source area of the 2018 Hokkaido Eastern Iburi Earthquake, Japan

Three dimensional S wave attenuation structure in and around source area of the 2018 Hokkaido Eastern Iburi Earthquake, Japan

... 180 s from S-wave arrival is the ...and source simultaneously with spatial variation in ...average S-wave velocity from ground surface to 20-m depth ...geology around the ... See full document

10

The performance of using an autoencoder for prediction and susceptibility assessment of landslides: A case study on landslides triggered by the 2018 Hokkaido Eastern Iburi earthquake in Japan

The performance of using an autoencoder for prediction and susceptibility assessment of landslides: A case study on landslides triggered by the 2018 Hokkaido Eastern Iburi earthquake in Japan

... study area, indicating the over-estimation of landslide susceptibility and low capacity in distin- guishing landslide-prone areas from stable ...the area under the curve of TPR and TNR, and TPR and FPR ... See full document

14

Coseismic changes in subsurface structure associated with the 2018 Hokkaido Eastern Iburi Earthquake detected using autocorrelation analysis of ambient seismic noise

Coseismic changes in subsurface structure associated with the 2018 Hokkaido Eastern Iburi Earthquake detected using autocorrelation analysis of ambient seismic noise

... Figure 6b shows the coseismic slip distribution esti- mated from strong motion records and hypocenters relocated by applying the double-difference method (Japan Meteorological Agency 2018). The aftershocks ... See full document

11

RETRACTED ARTICLE: Estimation of the source process and forward
simulation of long period ground motion of the 2018 Hokkaido Eastern Iburi, Japan,
earthquake

RETRACTED ARTICLE: Estimation of the source process and forward simulation of long period ground motion of the 2018 Hokkaido Eastern Iburi, Japan, earthquake

... point source with the mechanism and the seismic moment referring to F-net, and a smoothed ramp-type source time function with a 2-s ...direct S-wave pulse and later phases (Additional ... See full document

11

Seismic potential around the 2018 Hokkaido Eastern Iburi earthquake assessed considering the viscoelastic relaxation

Seismic potential around the 2018 Hokkaido Eastern Iburi earthquake assessed considering the viscoelastic relaxation

... velocity structure that contains low-velocity layer beneath the source region (Iwasaki et ...After three iterations, the RMS decreased from 0.437 to 0.135 s for the P-wave and from ... See full document

15

Geodetically estimated location and geometry of the fault plane involved in the 2018 Hokkaido Eastern Iburi earthquake

Geodetically estimated location and geometry of the fault plane involved in the 2018 Hokkaido Eastern Iburi earthquake

... the 2018 Hokkaido Eastern Iburi earthquake, the ground displacement fields were successfully ...the eastern side of an active fault, known as the Ishikari-Teichi-Toen fault zone ... See full document

9

The 2018 Hokkaido Eastern Iburi earthquake (MJMA = 6 7) was triggered by a strike slip faulting in a stepover segment: insights from the aftershock distribution and the focal mechanism solution of the main shock

The 2018 Hokkaido Eastern Iburi earthquake (MJMA = 6 7) was triggered by a strike slip faulting in a stepover segment: insights from the aftershock distribution and the focal mechanism solution of the main shock

... northeastern Japan island arcs ...intraplate earthquake immediately after the main shock by using data from a permanent local seismic network and found that aftershock depths were concentrated from 20 to 40 ... See full document

8

Three dimensional P  and S wave attenuation structures around the source region of the 2016 Kumamoto earthquakes

Three dimensional P and S wave attenuation structures around the source region of the 2016 Kumamoto earthquakes

... Kyushu Island is located in southwest Japan. The Phil- ippine Sea (PHS) plate is subducting beneath this region along the Nankai Trough. The active volcanoes men- tioned above are located along the volcanic front ... See full document

9

Electrical resistivity modeling around the Hidaka collision zone, northern Japan: regional structural background of the 2018 Hokkaido Eastern Iburi earthquake (Mw 6 6)

Electrical resistivity modeling around the Hidaka collision zone, northern Japan: regional structural background of the 2018 Hokkaido Eastern Iburi earthquake (Mw 6 6)

... NE Japan and Kurile arcs, is known to be an ideal region to study the evolution of island ...the 2018 Hokkaido Eastern Iburi earthquake (M w ...inland earthquake, and the ... See full document

10

Detection and interpretation of local surface deformation from the 2018 Hokkaido Eastern Iburi Earthquake using ALOS 2 SAR data

Detection and interpretation of local surface deformation from the 2018 Hokkaido Eastern Iburi Earthquake using ALOS 2 SAR data

... the 2018 Hokkaido Eastern Iburi Earthquake in northern Japan using satellite radar interferograms from the Advanced Land Observing Satellite ...main earthquake as well as ... See full document

17

Cause of destructive strong ground motion within 1–2 s in Mukawa town during the 2018 Mw 6 6 Hokkaido eastern Iburi earthquake

Cause of destructive strong ground motion within 1–2 s in Mukawa town during the 2018 Mw 6 6 Hokkaido eastern Iburi earthquake

... the 2018 Hokkaido eastern Iburi ...surface wave method in the dam- aged areas of the town of Mukawa, Hokkaido prefecture, ...6, 2018. The heavily damaged buildings were ... See full document

11

Characteristics of relocated hypocenters of the 2018 M6 7 Hokkaido Eastern Iburi earthquake and its aftershocks with a three dimensional seismic velocity structure

Characteristics of relocated hypocenters of the 2018 M6 7 Hokkaido Eastern Iburi earthquake and its aftershocks with a three dimensional seismic velocity structure

... the 2018 M6.7 Hokkaido Eastern Iburi earthquake and its surrounding area, using a three-dimensional seismic structure, the double-difference relocation ... See full document

11

Source rupture process of the 2018 Hokkaido Eastern Iburi earthquake deduced from strong motion data considering seismic wave propagation in three dimensional velocity structure

Source rupture process of the 2018 Hokkaido Eastern Iburi earthquake deduced from strong motion data considering seismic wave propagation in three dimensional velocity structure

... point source moment ten- sor was assumed for as the source term, and we used the moment tensor solution of F-net, ...The source parameters of this aftershock are summa- rized in Table ...the ... See full document

17

Characteristics of postseismic deformation following the 2003 Tokachi oki earthquake and estimation of the viscoelastic structure in Hokkaido, northern Japan

Characteristics of postseismic deformation following the 2003 Tokachi oki earthquake and estimation of the viscoelastic structure in Hokkaido, northern Japan

... Tokachi-oki earthquake is useful to dis- cuss a potential of future earthquakes along the Kurile ...tsunamigenic earthquake in the seventeenth century was estimated in the shallower part of the plate ... See full document

12

Study on 3D Thematic Map of Earthquake Emergency Based on GIS

Study on 3D Thematic Map of Earthquake Emergency Based on GIS

... surface three kinds of data, by giving these data to meet the seismic industry norms of the special symbols and color formation earthquake emergency information ...the earthquake industry, its own ... See full document

7

Assessment of Use of Microsatellite Polymorphism Analysis for Improving Spatial Distribution Tracking of Echinococcus multilocularis

Assessment of Use of Microsatellite Polymorphism Analysis for Improving Spatial Distribution Tracking of Echinococcus multilocularis

... shown three distinct genetic profiles for European, North American, and Japanese isolates, but no variability between individual samples of the respective foci has been found ...from Hokkaido Island, but no ... See full document

8

Resistivity structure around the focal area of the 2004 Rumoi Nanbu earthquake (M 6 1), northern Hokkaido, Japan

Resistivity structure around the focal area of the 2004 Rumoi Nanbu earthquake (M 6 1), northern Hokkaido, Japan

... geological structure support the ob- ...an earthquake. The Japan National Oil Corporation (1986) reported the physical prop- erties of the core samples and borehole logging (Table ... See full document

6

Resistivity structure around the hypocentral area of the 1984 Western Nagano Prefecture earthquake in central Japan

Resistivity structure around the hypocentral area of the 1984 Western Nagano Prefecture earthquake in central Japan

... Central Japan, in August 1976, and the first eruption of ...fecture earthquake of ...steady earthquake swarm activities which continued after the 1979 ...This earthquake caused heavy damage to ... See full document

12

Tectonomagnetic study in the eastern part of Hokkaido, NE Japan (II): Magnetic fields related with the 2003 Tokachi oki earthquake and the 2004 Kushiro oki earthquake

Tectonomagnetic study in the eastern part of Hokkaido, NE Japan (II): Magnetic fields related with the 2003 Tokachi oki earthquake and the 2004 Kushiro oki earthquake

... another earthquake will be triggered in the neighboring seismogenic ...dicted earthquake is hypothesized to occur off the Nemuro peninsula where the M ...7.9 earthquake occurred in 1894 (Fig. 2) ... See full document

6

Strong ground motions from an Mj 6 1 inland crustal earthquake in Hokkaido, Japan: the 2004 Rumoi earthquake

Strong ground motions from an Mj 6 1 inland crustal earthquake in Hokkaido, Japan: the 2004 Rumoi earthquake

... the source effect and the site ...The source effect is investigated by constructing the source model that explains the broad-band strong-motion records at four stations around the epicenter ... See full document

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