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[PDF] Top 20 Coseismic slip distribution of the 2005 off Miyagi earthquake (M7 2) estimated by inversion of teleseismic and regional seismograms

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Coseismic slip distribution of the 2005 off Miyagi earthquake (M7 2) estimated by inversion of teleseismic and regional seismograms

Coseismic slip distribution of the 2005 off Miyagi earthquake (M7 2) estimated by inversion of teleseismic and regional seismograms

... For the geometrical parameters of the fault model, the AQUA-CMT values of the National Research Institute of Earth Science and Disaster Prevention were used: strike 198.2 ◦ , dip 22.2 ◦ , slip 81.9 ◦ . The ... See full document

6

Hypocenter distribution of the main  and aftershocks of the 2005 Off Miyagi Prefecture earthquake located by ocean bottom seismographic data

Hypocenter distribution of the main and aftershocks of the 2005 Off Miyagi Prefecture earthquake located by ocean bottom seismographic data

... occur off the plane of the mainshock rupture, possibly within the sub- ducting oceanic ...area estimated from the analysis of the teleseismic data extends more to the east than the actual location of ... See full document

6

Co  and post seismic slip associated with the 2005 Miyagi oki earthquake (M7 2) as inferred from GPS data

Co and post seismic slip associated with the 2005 Miyagi oki earthquake (M7 2) as inferred from GPS data

... Co-seismic slip distributions both from the waveform in- version by Yaginuma et ...The slip area larger than 0.3 m, which was geodetically estimated and shown by a green contour line, indicates a ... See full document

6

Fault model of the 2005 Fukuoka ken Seiho oki earthquake estimated from coseismic deformation observed by GPS and InSAR

Fault model of the 2005 Fukuoka ken Seiho oki earthquake estimated from coseismic deformation observed by GPS and InSAR

... which slip is ...nonlinear inversion method de- veloped by Matsu’ura and Hasegawa (1987) to estimate pa- rameters of a rectangular ...and slip), we determine the offset in LOS dis- placement to ... See full document

6

A preliminary fault model of the 2003 July 26, M6 4 northern Miyagi earthquake, northeastern Japan, estimated from joint inversion of GPS, leveling, and InSAR data

A preliminary fault model of the 2003 July 26, M6 4 northern Miyagi earthquake, northeastern Japan, estimated from joint inversion of GPS, leveling, and InSAR data

... Figs. 2, 3, 4, and ...(Figs. 2 and 3), leveling ...uniform slip on the segments and complex geometry of the ...fault slip in the southern extension of Segment 1. Variable slip ... See full document

7

Coseismic and Postseismic Displacement of 2011 Mw 6 8 Tarlay Earthquake, Myanmar using InSAR Techniques and Inversion Analysis

Coseismic and Postseismic Displacement of 2011 Mw 6 8 Tarlay Earthquake, Myanmar using InSAR Techniques and Inversion Analysis

... To refine the result of Single-patch model, the planar fault is divided into smaller rectangular areas, each of which may assume different slip values. This model provides more realistic values of slip than ... See full document

14

Seismic moment of the 1891 Nobi, Japan, earthquake estimated from historical seismograms

Seismic moment of the 1891 Nobi, Japan, earthquake estimated from historical seismograms

... Nobi earthquake was the great- est inland earthquake ever experienced on the Japanese Is- ...first estimated as ...the distribution of seismic in- tensities around the epicentral ...great ... See full document

7

Coseismic displacements and slip distribution from GPS and leveling observations for the 2006 Peinan earthquake (Mw 6 1) in southeastern Taiwan

Coseismic displacements and slip distribution from GPS and leveling observations for the 2006 Peinan earthquake (Mw 6 1) in southeastern Taiwan

... the inversion with only the CGPS sites described in the previous ...est slip of about ...fault slip on the northern portion is mainly left-lateral, while it is pri- marily up-dip on the south portion ... See full document

20

Causes of the N–S compressional aftershocks of the E–W compressional 2008 Iwate–Miyagi Nairiku earthquake (M7 2) in the northeastern Japan arc

Causes of the N–S compressional aftershocks of the E–W compressional 2008 Iwate–Miyagi Nairiku earthquake (M7 2) in the northeastern Japan arc

... times estimated from the cross- correlation of the seismic waveforms may have large esti- mation errors due to the mismatching of the phases by one cycle which is known as “cycle ...an earthquake is lower ... See full document

13

Source modeling of the 2005 off shore Miyagi prefecture, Japan, earthquake (MJMA=7 2) using the empirical Green’s function method

Source modeling of the 2005 off shore Miyagi prefecture, Japan, earthquake (MJMA=7 2) using the empirical Green’s function method

... and 2 provide detailed information on the mainshock and the EGF-event, respec- ...were estimated roughly from the displacement source spectra calculated by the borehole data of KiK-net, which are not ... See full document

6

Slip distribution of the 1973 Nemuro oki earthquake estimated from the re examined geodetic data

Slip distribution of the 1973 Nemuro oki earthquake estimated from the re examined geodetic data

... includes coseismic deformation as well as post- seismic and interseismic ...terseismic, coseismic, and postseismic deformations were continuously observed in Hokkaido ...the slip distribution ... See full document

12

Analysis of co-seismic displacement and Coulomb stress change after Nepal earthquake on 25 April, 2015

Analysis of co-seismic displacement and Coulomb stress change after Nepal earthquake on 25 April, 2015

... The earthquake occurred in the Himalayan thrust wedge near the basal decollement which defines the lower boundary of the thrust wedge and is referred to as the Main Himalayan Thrust fault (MHT), as in ... See full document

8

Compound fault rupture during the 2004 off the Kii Peninsula earthquake (M 7 4) inferred from highly resolved coseismic sea surface deformation

Compound fault rupture during the 2004 off the Kii Peninsula earthquake (M 7 4) inferred from highly resolved coseismic sea surface deformation

... thrust slip along a fault parallel to the trough ...2004 off the Kii peninsula earthquake is still ...questions, inversion analyses us- ing seismic, tsunami, and geodetic data are useful ... See full document

6

The role of space-based observation in understanding and responding to active tectonics and earthquakes

The role of space-based observation in understanding and responding to active tectonics and earthquakes

... fault slip-rate and the depth to which faults are locked by friction in the interseismic period 75 , with strong assumptions of a known slip direction imposed by the one- dimensional nature of these ... See full document

16

Source process of the 1923 Kanto earthquake inferred from historical geodetic, teleseismic, and strong motion data

Source process of the 1923 Kanto earthquake inferred from historical geodetic, teleseismic, and strong motion data

... present slip dis- tributions suggests few aftershocks around the larger east- ern asperity as expected from the established theory on af- tershock patterns and main shock faulting ...Tokachi-oki earthquake ... See full document

10

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

... that estimated by the inversion of the GPS data with fixed fault dip and strike based on the after- shock distribution (Tobita et ...that estimated by the coastal verti- cal crustal deformation ... See full document

11

Simultaneous estimation of the dip angles and slip distribution on the faults of the 2016 Kumamoto earthquake through a weak nonlinear inversion of InSAR data

Simultaneous estimation of the dip angles and slip distribution on the faults of the 2016 Kumamoto earthquake through a weak nonlinear inversion of InSAR data

... the slip distribution on it, based on Akaike’s Bayes- ian information criterion (ABIC) by regarding the dip angle as a ...the slip distribu- tion, even though a complicated rupture like the Kuma- ... See full document

10

Coseismic fault model of the 2008 Iwate Miyagi Nairiku earthquake deduced by a dense GPS network

Coseismic fault model of the 2008 Iwate Miyagi Nairiku earthquake deduced by a dense GPS network

... sai, 2005), which is a GPS processing suite developed in Japan, to process the data using the kinematic PPP ...are estimated using an extended Kalman filter ...were estimated using a strictly ... See full document

5

Pore pressure distribution in the focal region of the 2008 M7 2 Iwate Miyagi Nairiku earthquake

Pore pressure distribution in the focal region of the 2008 M7 2 Iwate Miyagi Nairiku earthquake

... pressure distribution in the focal region of the 2008 Iwate-Miyagi Nairiku earthquake was investigated through an analysis of the diversity of focal ...The estimated stress orientation is ... See full document

7

Seismic dynamo effects associated with the M7 1 earthquake of 26 May 2003 off Miyagi Prefecture and the M6 4 earthquake of 26 July 2003 in northern Miyagi Prefecture, NE Japan

Seismic dynamo effects associated with the M7 1 earthquake of 26 May 2003 off Miyagi Prefecture and the M6 4 earthquake of 26 July 2003 in northern Miyagi Prefecture, NE Japan

... The sampling rate for continuous MT observations is 24 Hz which is fairly slower than that for seismic records, 100 Hz, but this is not very crucial in view of errors in the ar- rival time estimation for the area ... See full document

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