Add to ORKGThe abrupt changes of the crustal strains during the earthquakes have been observed with some components of highly sensitive extensometers. The relations between the seismic magnitude M and the coefficient k of the transmission of the abrupt change have been obtained as log k=l.l7M+4.52. Moreover, the relations between the magnitude M and those of the radius of the fault area ro and the total released energy of the crustal strain Er have been calculated as, 1
Abstract The 2011 Tohoku-Oki earthquake, of moment magnitude (M w) 9.0, occurred on March 11, 2011, ...
International audienceStudies of mechanical responses of the Earth crust to large earthquakes can pr...
Abstract:Co-seismic strain changes of the Wenchuan Mw7. 9 earthquake recorded with three four-compon...
We have sometimes found sudden changes of the crustal deformation in the observations with extensome...
On the basis of stress accumulation between two large earthquakes the maximum strain rate can be est...
The observations of vibrational strains in the earthquakes by means of these strain seismographshave...
The great Sumatra-Andaman earthquake of December 26, 2004 is studied by using extensometer (strain-m...
At Osakayama, the observations of changes in strains and tiltings of the groundhave been constantly ...
A remarkable strain step was recorded by the strainmeter at the Inuyama Crustral Movement Observator...
Results from repetitional measurements of six base-line networks founded in the western Japanby a ge...
International audienceStudies of mechanical responses of the Earth crust to large earthquakes can pr...
International audienceStudies of mechanical responses of the Earth crust to large earthquakes can pr...
International audienceStudies of mechanical responses of the Earth crust to large earthquakes can pr...
International audienceStudies of mechanical responses of the Earth crust to large earthquakes can pr...
International audienceStudies of mechanical responses of the Earth crust to large earthquakes can pr...
Abstract The 2011 Tohoku-Oki earthquake, of moment magnitude (M w) 9.0, occurred on March 11, 2011, ...
International audienceStudies of mechanical responses of the Earth crust to large earthquakes can pr...
Abstract:Co-seismic strain changes of the Wenchuan Mw7. 9 earthquake recorded with three four-compon...
We have sometimes found sudden changes of the crustal deformation in the observations with extensome...
On the basis of stress accumulation between two large earthquakes the maximum strain rate can be est...
The observations of vibrational strains in the earthquakes by means of these strain seismographshave...
The great Sumatra-Andaman earthquake of December 26, 2004 is studied by using extensometer (strain-m...
At Osakayama, the observations of changes in strains and tiltings of the groundhave been constantly ...
A remarkable strain step was recorded by the strainmeter at the Inuyama Crustral Movement Observator...
Results from repetitional measurements of six base-line networks founded in the western Japanby a ge...
International audienceStudies of mechanical responses of the Earth crust to large earthquakes can pr...
International audienceStudies of mechanical responses of the Earth crust to large earthquakes can pr...
International audienceStudies of mechanical responses of the Earth crust to large earthquakes can pr...
International audienceStudies of mechanical responses of the Earth crust to large earthquakes can pr...
International audienceStudies of mechanical responses of the Earth crust to large earthquakes can pr...
Abstract The 2011 Tohoku-Oki earthquake, of moment magnitude (M w) 9.0, occurred on March 11, 2011, ...
International audienceStudies of mechanical responses of the Earth crust to large earthquakes can pr...
Abstract:Co-seismic strain changes of the Wenchuan Mw7. 9 earthquake recorded with three four-compon...