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1 National Geophysical Research
Institute
Hyderabad 500007, India
(S.P.)
2 Department of Geophysics and
Geology
University of Leipzig
D-04103 Leipzig, Germany
(U.W.,
M.K.)
We apply the energy transfer theory of 3D multiple isotropic scattering
to analyze seismogram envelopes of the 2001 Bhuj earthquake of India. We
synthesized
the S-wave coda envelopes by using a numerical Monte Carlo method. Our
model is described by total scattering coefficient g, intrinsic
absorption coefficient
b, spectral source energy S, and site factors Z.
Isotropic source radiation and acoustic
wave propagation were assumed. We inverted the observed coda envelopes of 10
aftershocks (ML
4) using the grid search for g,
least-squares inversion for b, and S
between 1 and 24 Hz. Parameter g does not show significant frequency
dependency
and averages to 0.01 1/km. This corresponds to a mean free path of 100 km.
Parameter
b shows weak frequency dependency, increasing with frequency. Its value
ranges
from 0.02 1/sec to 0.05 1/sec. Consequently, the frequency dependency of
intrinsic
attenuation takes the power-law form of Qi(f)
= 280f0.72. The source energy is
largely consistent with the well-known
2-source model
and the seismic moment is
comparable to estimates using standard empirical relations between seismic
moment
and local magnitude. We also inverted the envelopes for site-amplification
factors Z.
The values of Z range from 0.5 to 1.75 with no clear frequency
dependence, which
is consistent with the geology of the region, as the stations were deployed on
hard-
rock sites.
This article has been cited by other articles:
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S. Padhy Characteristics of Body-Wave Attenuations in the Bhuj Crust Bulletin of the Seismological Society of America, December 1, 2009; 99(6): 3300 - 3313. [Abstract] [Full Text] [PDF] |
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S. Padhy Inversion of Seismogram Envelopes Using a Multiple Isotropic Scattering Model in Garhwal Himalaya Bulletin of the Seismological Society of America, April 1, 2009; 99(2A): 726 - 740. [Abstract] [Full Text] [PDF] |
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