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[PDF] Top 20 Strong ground motion recorded by high rate sampling GPS at the closest site to the 2003 Tokachi oki earthquake

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Strong ground motion recorded by high rate sampling GPS at the closest site to the 2003 Tokachi oki earthquake

Strong ground motion recorded by high rate sampling GPS at the closest site to the 2003 Tokachi oki earthquake

... that GPS observation provides data on strong ground motion generated by magnitude 8 earth- quake in a very short ...between GPS displacements and integrated accelerograms is another ... See full document

5

Consistency of PPP GPS and strong motion records: case study of Mw9 0 Tohoku Oki 2011 earthquake

Consistency of PPP GPS and strong motion records: case study of Mw9 0 Tohoku Oki 2011 earthquake

... the GPS and the strong-motion records is made using data collected by very close spaced sites of the GPS and strong-motion ...At high frequency (> 1Hz), in order to ... See full document

20

The potential of high rate GPS for strong ground motion assessment

The potential of high rate GPS for strong ground motion assessment

... of GPS displacement time series established using various software packages (Bern- ese, GAMIT, and RTKLIB), GPS datasets from different networks (GNSS Earth Observation Network System [GEONET]; ... See full document

12

Measuring ground deformations with 1 Hz GPS data: the 2003 Tokachi oki earthquake (preliminary report)

Measuring ground deformations with 1 Hz GPS data: the 2003 Tokachi oki earthquake (preliminary report)

... The GPS stations are located 70–240 km away from the epicenter. GPS data clearly captured rapid co-seismic ground ...a GPS station 70 km away from the epicenter, coseismic displacements ... See full document

5

Afterslip distribution following the 2003 Tokachioki earthquake: An estimation based on the Green’s functions for an inhomogeneous elastic space with subsurface structure

Afterslip distribution following the 2003 Tokachioki earthquake: An estimation based on the Green’s functions for an inhomogeneous elastic space with subsurface structure

... mation of afterslip distribution, since the subsurface struc- ture of any region, especially that in and around Japan, is more or less inhomogeneous, and such inhomogeneity should affect, to a certain extent, the surface ... See full document

10

Investigation of strong earthquake ground motion

Investigation of strong earthquake ground motion

... v TABLE OF CONTENTS PART I II TITLE PAGE INTRODUCTION 1 PATTERN OF ENERGY RELEASE DURING THE IMPERIAL VALLEY, CALIFORNIA EARTHQUAKE OF 1940 3 RELATIVT!: AMPLITUDES AND SPECTRAL PROPERTIE[r] ... See full document

153

Surface latent heat flux and nighttime LF anomalies prior to the =8.3 Tokachi-Oki earthquake

Surface latent heat flux and nighttime LF anomalies prior to the =8.3 Tokachi-Oki earthquake

... that strong disturbances in VLF/LF signals occur during daytime due to additional ion- ization of the lower ionosphere by solar X-ray ...Very strong (about 10 times over regular signal level, measured in ... See full document

6

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

... the 2003 event suggests 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 ... See full document

6

Deep seismic activities preceding the three large ‘shallow’ earthquakes off south east Hokkaido, Japan—the 2003 Tokachi oki earthquake, the 1993 Kushiro oki earthquake and the 1952 Tokachi oki earthquake

Deep seismic activities preceding the three large ‘shallow’ earthquakes off south east Hokkaido, Japan—the 2003 Tokachi oki earthquake, the 1993 Kushiro oki earthquake and the 1952 Tokachi oki earthquake

... large earthquake in 1950 (M ...focus earthquake occurred when it reaches at some depth, and it was followed shortly afterward by a great shallow ...deep-focus earthquake to the great shallow ... See full document

5

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

... series. We obtained the amplitude of the offset as the dif- ference between coordinates averaged for 10 days just before and after the earthquakes. We finally modeled the corrected time series as a sum of a piecewise ... See full document

12

GPS observation of the first month of postseismic crustal deformation associated with the 2003 Tokachi oki earthquake (MJMA
               8 0), off southeastern Hokkaido, Japan

GPS observation of the first month of postseismic crustal deformation associated with the 2003 Tokachi oki earthquake (MJMA 8 0), off southeastern Hokkaido, Japan

... al., 2003). These visible ground uplifts requested the sizable slips at the downdip extension of the seismogenic part, where we believe that plate interface is ... See full document

6

Aftershock observation of the 2003 Tokachi oki earthquake by using dense ocean bottom seismometer network

Aftershock observation of the 2003 Tokachi oki earthquake by using dense ocean bottom seismometer network

... the 2003 Tokachi-oki Earthquake, forty-seven OBSs and two OBPs were deployed at thirty-eight sites from September 30 to November 20, 2003, in the source region of the main- ...with ... See full document

6

Spatial distribution for moment tensor solutions of the 2003 Tokachi oki earthquake (MJMA
               = 8 0) and aftershocks

Spatial distribution for moment tensor solutions of the 2003 Tokachi oki earthquake (MJMA = 8 0) and aftershocks

... a rate of about 90 mm/year (Heki, 1989) ...off Tokachi region. Hasegawa et al. (1994) and Kat- sumata (2003) revealed the geometry of double-planed deep seismic zone of deep and intermediate-depth ... See full document

6

A Study of High Frequency Strong Ground Motion from the San Fernando Earthquake

A Study of High Frequency Strong Ground Motion from the San Fernando Earthquake

... motion generally involved only correlations between earthquake magnitude and recorded peak ground motion values, and did not consider details of the rupture mechanism and the geology of [r] ... See full document

277

Disturbances in VHF/UHF telemetry links as a possible effect of the 2003 Hokkaido Tokachi-oki earthquake

Disturbances in VHF/UHF telemetry links as a possible effect of the 2003 Hokkaido Tokachi-oki earthquake

... The usual noise level in VHF/UHF band is ∼ 7 dBµV/m in an area with high city noises, ∼ 3 dBµV/m in residen- tial areas and ∼ 2 dBµV/m in the mountaneous areas. On the supposition that the Ministry would adopt the ... See full document

5

Low frequency events occurred during the sequence of aftershock activity of the 2003 Tokachi Oki earthquake; a dynamic process of the tectonic erosion by subducted seamount

Low frequency events occurred during the sequence of aftershock activity of the 2003 Tokachi Oki earthquake; a dynamic process of the tectonic erosion by subducted seamount

... the high sensitivity accelerometer observed at N.SAMH with the time period of one hour. There are a few seismograms of normal aftershock events in the first half of the one hour. Around 3:37 am and 3:46 am, very ... See full document

5

Spatial pattern in stress drops of moderate-sized earthquakes on the Pacific Plate off the south-east of Hokkaido, Japan: implications for the heterogeneity of frictional properties

Spatial pattern in stress drops of moderate-sized earthquakes on the Pacific Plate off the south-east of Hokkaido, Japan: implications for the heterogeneity of frictional properties

... values of stress drop to the slip distribution of the earth- quake. They found that small earthquakes around large slip patches of the main shock were likely to have larger values of stress drop. They concluded that the ... See full document

12

Tsunami run up heights of the 2003 Tokachi oki earthquake

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

7

Real time characterization of large earthquakes using the predominant period derived from 1Hz GPS data

Real time characterization of large earthquakes using the predominant period derived from 1Hz GPS data

... context, GPS waveforms may be useful to EEW systems for at least two reasons: First, GPS time series, due to their lower sensitivity ...2017). GPS-based EEW systems could thus be operated ... See full document

10

Source rupture process of the 2003 Tokachi oki earthquake determined by joint inversion of teleseismic body wave and strong ground motion data

Source rupture process of the 2003 Tokachi oki earthquake determined by joint inversion of teleseismic body wave and strong ground motion data

... 26, 2003 September 25, 2003 at 19:50 (GMT), a great thrust earthquake occurred off Tokachi (Tokachi-oki), Hokkaido, Northern ...The earthquake information initially ... See full document

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