IISEE’s CMTs, Aftershock
Distributions, Fault planes, and Rupture processes for recent large earthquakes
in the world [Japanese version]
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[Outline]
The IISEE has started a project to determine the following
earthquake information for recent large (Mw≧7.2) earthquakes in the world by the analytical
techniques developed by the IISEE staff members and visiting researchers.
n
Centroid moment tensor
Centroid moment tensors
are determined analyzing long period body wave data recorded at GSN (Global
Seismological Network) stations.
u
Period: 1994 - 2007
u
Analytical method: Grid search approach by Hara (2004, 2005)
u
Principal Investigator: Tatsuhiko
Hara (IISEE. E-mail: thara at kenken.go.jp)
n
Aftershock distribution and corresponding fault plane
Aftershocks
including mainshock and foreshocks are relocated
using P-wave arrivals from International Seismological Centre (ISC) CD-ROMs.
Then, the corresponding fault plane is determined based on the obtained
aftershock distribution (nodal planes are taken from the Global CMT catalog).
u
Period: January 1994 – October 2004
u
Analytical method: The modified joint hypocenter
determination method (MJHD. Hurukawa and Imoto, 1992; Hurukawa, 1995; Hurukawa et al., 2008)
u
Principal Investigator: Nobuo
Hurukawa (IISEE. E-mail: hurukawa at kenken.go.jp)
n
Rupture process
Earthquake rupture processes
are determined analyzing broadband waveform data recorded at GSN (Global
Seismological Network) stations. The above aftershock analyses are referred to
set up earthquake fault planes.
u
Period: January 1994 – October 2004
u
Analytical method: Waveform inversion considering covariance
components in inversion analyses of densely sampled observed data by Yagi and Fukahata (2008)
u
Principal Investigator: Yuji Yagi
(
In addition, we
have developed software to perform strong ground motion simulation for seismic
bedrock using stochastic Green’s function method.
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Seismology and Earthquake Engineering, Building Research Institute All Rights
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