[PDF] Top 20 Slip model of the 2008 Mw 7 9 Wenchuan (China) earthquake derived from co seismic GPS data
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Slip model of the 2008 Mw 7 9 Wenchuan (China) earthquake derived from co seismic GPS data
... improved from being an averaged slip estimation of one or several fault planes to slip distribution estimation of multiple finite discrete fault patches, based on sufficient near-field constraints ... See full document
6
Rise time and source duration of the 2008 MW 7 9 Wenchuan (China) earthquake as revealed by Rayleigh waves
... the 2008 Wenchuan earthquake were studied in a rupture directivity analysis by simultaneously inverting the period of the rst Fourier spectral-node and the 100-s phase-delay time of the Rayleigh ... See full document
8
Remotely triggered seismicity in north China following the 2008 Mw 7 9 Wenchuan earthquake
... small-amplitude seismic waves can trig- gered earthquakes at teleseismic distances (Hill and Pre- jean, 2007; and references ...physical model over others in this study, due to the relatively small number ... See full document
6
The Mw 7 9, 12 May 2008 Sichuan earthquake rupture measured by sub pixel correlation of ALOS PALSAR amplitude images
... (USGS, 2008) between two major faults of the Long- men Shan thrust system, the Wenchuan and Beichuan faults ...(SAR) from the PALSAR sensor ... See full document
5
Key factors influencing the mechanism of rapid and long runout landslides triggered by the 2008 Wenchuan earthquake, China
... the seismic record to Donghekou slide, modifi- cations would have to be ...the seismic intensity at the Donghekou slide can be treated as the same as that recorded in SFB ...same seismic intensity ... See full document
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Coseismic slip distribution of the 2011 off the Pacific coast of Tohoku Earthquake (M 9 0) estimated based on GPS data—Was the asperity in Miyagi oki ruptured?
... performed seismic waveform inver- sion for the 2005 event to estimate the coseismic slip distri- bution and found that it also corresponds to the southeastern part of the 1978 rupture ...1978 ... See full document
6
Characteristics and classification of landslide dams associated with the 2008 Wenchuan earthquake
... main deposition zone is mainly composed of fine rock fragments and debris mixed with large blocks and boulders with grain sizes varying from 2 m to 10 m. The middle and bottom layers did not strongly disaggregate, ... See full document
15
Improved Methodology for Seismic Estimation of Highway Based on Wenchuan Earthquake
... In retaining structure, the reinforced retaining wall, anti-slide pile and bolt type retaining wall, which perform well in earthquake, are classified as seismic favorable type. As for slope protection, it ... See full document
6
Analysis of spatiotemporal variations in middle-tropospheric to upper-tropospheric methane during the Wenchuan Ms = 8.0 earthquake by three indices
... the Wenchuan earthquake (12 May 2008) using AIRS re- trieval data and discussed the methane anomaly ...in 2008, with an average increase of ...the earthquake broke the ... See full document
14
Geochemistry of soil gas in the seismic fault zone produced by the Wenchuan Ms 8.0 earthquake, southwestern China
... because co- seismic ruptures usually enhance the permeability of rock and soil, favoring gas emission and resulting in ‘’ halo ’’ ...resulted from the dif- ferences in fault and soil features ... See full document
10
A fault model of the 1995 Kobe earthquake derived from the GPS data on the Akashi Kaikyo Bridge and other datasets
... The pattern of most horizontal displacements in Fig. 2 in- dicates right-lateral strike-slip along the two fault segments like the focal mechanism, but 3P and 4A were displaced westward against 1A and 2P in ... See full document
9
Outline of the 2011 off the Pacific coast of Tohoku Earthquake (Mw 9 0) —Earthquake Early Warning and observed seismic intensity—
... issued Earthquake Early Warning (EEW) announcements to the general public of the Tohoku district and then the warning was automatically broadcast through TV, radios and cellular phone ...district. Seismic ... See full document
5
Near field TEC response to the main shock of the 2008 Wenchuan earthquake
... an earthquake. The authors used GPS-arrays, consisted of three sites, the distances between which do not exceed about one-half the wavelength of the perturbation (D1 ... See full document
6
Focal mechanism and slip history of the 2011 Mw 9 1 off the Pacific coast of Tohoku Earthquake, constrained with teleseismic body and surface waves
... downloaded from the IRIS data center provided by global seismograph network (GSN) and other networks such as GEOSCOPE, GEOFON, New China Digital Seismograph Net- work, ...The GPS coseismic ... See full document
6
Co seismic surface deformation of the 2011 off the Pacific coast of Tohoku Earthquake: Spatio temporal EOF analysis of GPS data
... The co-seismic strain field derived from the EOF solu- tions can provide further insights into a synoptic spatio- temporal scenario of surface ... See full document
6
Assessment of risks of loose landslide deposits formed by the 2008 Wenchuan earthquake
... path from the epicenter, Yingxiu, to the Research and Con- servation Centre for Giant Panda at Wolong ...PR303 from milestone K1 to K18 as shown in ... See full document
12
Preceding seismic activity and slow slip events in the source area of the 2011 Mw 9.0 Tohoku-Oki earthquake: a review
... maximum slip at the two large slip patches is esti- mated to be 50–65 m ...large slip would take several hundred years to accumulate and the two large slip patches must have been locked for ... See full document
13
Possible large near trench slip during the 2011 Mw 9 0 off the Pacific coast of Tohoku Earthquake
... of co-seismic slip in large earthquakes is also impor- tant for consideration of how stresses are communicated to the trench-slope and outer rise intraplate environments, and the potential for ... See full document
6
Possibility of Mw 9 0 mainshock triggered by diffusional propagation of after slip from Mw 7 3 foreshock
... to earthquake generation, in order to accomplish such a pre- diction we need to know beforehand the locations of cou- pled patches and their tectonic stress ...these data and to translate them into physical ... See full document
5
Coseismic displacements and slip distribution from GPS and leveling observations for the 2006 Peinan earthquake (Mw 6 1) in southeastern Taiwan
... second model, we used the identical fault geome- try as determined by the inversion with only the CGPS sites described in the previous ...the model pre- dictions to GPS and leveling measurements are ... See full document
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