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[PDF] Top 20 Radiated energy from the Noto Hanto, Japan, earthquake of March 25, 2007, and its aftershock

Has 10000 "Radiated energy from the Noto Hanto, Japan, earthquake of March 25, 2007, and its aftershock" found on our website. Below are the top 20 most common "Radiated energy from the Noto Hanto, Japan, earthquake of March 25, 2007, and its aftershock".

Radiated energy from the Noto Hanto, Japan, earthquake of March 25, 2007, and its aftershock

Radiated energy from the Noto Hanto, Japan, earthquake of March 25, 2007, and its aftershock

... This earthquake is a shallow reverse-faulting ...an aftershock whose hypocenter is very close to that of the main shock to in- vestigate the scale-dependence of e ˜ for these ... See full document

6

Site amplification and strong ground motion of the 2007 Noto Hanto, Japan, earthquake estimated from aftershock observation

Site amplification and strong ground motion of the 2007 Noto Hanto, Japan, earthquake estimated from aftershock observation

... the 2007 Noto Hanto earthquake, Monzen, Anamizu, and Wajima, are examined using aftershock records observed at eight temporary seismic stations installed just after the mainshock and at ... See full document

7

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

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

... the Noto Hanto earthquake provide an excellent opportunity to examine earthquake triggering associated with a blind thrust ...The aftershock zone rapidly expanded into a ‘butterfly ... See full document

6

Magnetotelluric observations around the focal region of the 2007 Noto Hanto Earthquake (Mj 6 9), Central Japan

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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Relationship between coseismic slip and static stress drop of similar aftershocks of the 2007 Noto Hanto earthquake

Relationship between coseismic slip and static stress drop of similar aftershocks of the 2007 Noto Hanto earthquake

... the 2007 Noto Hanto earthquake, central Japan, and have examined the relationship between the coseismic slip of the mainshock and the static stress drop of the similar ...ranges ... See full document

8

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

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 Noto Peninsula during this rifting, those normal faults turned to reverse faults after the cease of the rifting due to the compressive stress associated with the forearc subduction (Katagawa et ...of ... See full document

11

Relation between similar aftershocks and ruptured asperity of a large inland earthquake: Example of the 2007 Noto Hanto earthquake

Relation between similar aftershocks and ruptured asperity of a large inland earthquake: Example of the 2007 Noto Hanto earthquake

... T. Iwasaki, T. Kanazawa, S. Watanabe, T. Haneda, M. Kobayashi, K. Miura, R. Miura, K. Tagami, I. Ogino, M. Saka, A. Watanabe, K. Miyakawa, K. Katsumata, H. Takahashi, M. Kasahara, R. Honda, T. Maeda, M. Ichiyanagi, T. ... See full document

5

Does the 2007 Noto Hanto earthquake reveal a weakness in the Japanese national seismic hazard map that could be remedied with geological data?

Does the 2007 Noto Hanto earthquake reveal a weakness in the Japanese national seismic hazard map that could be remedied with geological data?

... Abundant aftershocks have been recorded along the ENE-striking block-bounding faults, F14, F15, and F16 (Toda, 2008). Focal mechanisms of the moderate-sized aftershocks also suggest that the faulting mechanisms are ... See full document

6

Three dimensional velocity structure in the source region of the Noto Hanto Earthquake in 2007 imaged by a dense seismic observation

Three dimensional velocity structure in the source region of the Noto Hanto Earthquake in 2007 imaged by a dense seismic observation

... relocated aftershock hypocenters determined by dou- ble-difference tomography, shown as circles scaled to earthquake mag- nitude and colored to ...present earthquake are drawn as thick ... See full document

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Rupture process of the 2007 Noto Hanto earthquake: waveform inversion using empirical Green’s function

Rupture process of the 2007 Noto Hanto earthquake: waveform inversion using empirical Green’s function

... the 2007 Noto Hanto earthquake is relatively large and some of the stations which recorded the earthquake are lo- cated relatively close to the fault plane ...contributions from ... See full document

6

Source model of the 2007 Noto Hanto earthquake (Mw 6 7) for estimating broad band strong ground motion

Source model of the 2007 Noto Hanto earthquake (Mw 6 7) for estimating broad band strong ground motion

... on March 25, 2007 occurred west off the Noto penin- sula, ...a Japan Me- teorological Agency (JMA) seismic intensity of 6-upper struck Wajima, Anamizu, and Nanao in the northern part of ... See full document

6

Highly resolved distribution of aftershocks of the 2007 Noto Hanto Earthquake by a dense seismic observation

Highly resolved distribution of aftershocks of the 2007 Noto Hanto Earthquake by a dense seismic observation

... Sakai, S., A. Kato, E. Kurashimo, T. Iidaka, T. Igarashi, N. Hirata, T. Iwasaki, T. Kanazawa, S. Watanabe, T. Haneda, M. Kobayashi, K. Miura, R. Miura, K. Tagami, I. Ogino, M. Saka, A. Watanabe, K. Miyakawa, K. ... See full document

6

Gravity anomalies and the geologic block structures in and around the aftershock area of the 2007 Noto Hanto Earthquake

Gravity anomalies and the geologic block structures in and around the aftershock area of the 2007 Noto Hanto Earthquake

... shows aftershock distributions provided by Japan Meteorological Agency, and its vertical cross- sections projected approximately perpendicular to the earthquake ...the aftershock is ... See full document

5

Aftershock observation of the Noto Hanto earthquake in 2007 using ocean bottom seismometers

Aftershock observation of the Noto Hanto earthquake in 2007 using ocean bottom seismometers

... the 2007 Noto Hanto earthquake, strongly shock some regions of the Ishikawa prefecture, with a maximum seis- mic intensity of 6 Upper on the JMA scales, one person was killed and more than 350 ... See full document

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Characterization of the 2007 Noto Hanto, Japan, earthquake

Characterization of the 2007 Noto Hanto, Japan, earthquake

... calculated from the derived slip distribution exceeded 16 MPa for the major asperity, and the minor asperity has a similar maximum ...of radiated energy to seismic moment was also estimated for the ... See full document

6

Numerical simulation of the tsunami generated by the 2007 Noto Hanto Earthquake and implications for unusual tidal surges observed in Toyama Bay

Numerical simulation of the tsunami generated by the 2007 Noto Hanto Earthquake and implications for unusual tidal surges observed in Toyama Bay

... that occurred on 25 March 2007 near the Noto Peninsula on the northwest coast of Honshu Island, Japan. Our numerical simulation reproduced well the behaviors of the tsunami as recorded ... See full document

6

Postseismic displacements following the 2007 Noto peninsula earthquake detected by dense GPS observation

Postseismic displacements following the 2007 Noto peninsula earthquake detected by dense GPS observation

... the 2007 Noto peninsula earthquake since March 25, 2007, in order to detect postseismic ...the aftershock zone for this ... See full document

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Source processes of the foreshock, mainshock and largest aftershock in the 2003 Miyagi ken Hokubu, Japan, earthquake sequence

Source processes of the foreshock, mainshock and largest aftershock in the 2003 Miyagi ken Hokubu, Japan, earthquake sequence

... no aftershock before the main- shock ...between aftershock patterns and distributions of co- seismic slip and stated that aftershocks occur mostly outside of or near the edges of main slip ... See full document

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Observation of ground motions of aftershocks of the 2007 Noto Hanto earthquake in Monzenmachi, the Wajima city, for estimation of site amplification

Observation of ground motions of aftershocks of the 2007 Noto Hanto earthquake in Monzenmachi, the Wajima city, for estimation of site amplification

... comments from two reviewers are ac- knowledged to have improved the ...the 2007 Noto Hanto Earthquake from the Ministry of Education, Culture, Sports, Sci- ence and Technology ... 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

Rupture process during the 2007 Noto Hanto earthquake (MJMA 6 9) and strong motion simulation in the source region

... until its neighbor nearest to the rup- ture initiation point has failed (Ihml´e, ...searched from a set of samples repeatedly accepted in the displacement inversion below the “critical temperature” during ... See full document

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