Title of article :
A Study of Source Parameters, Site Amplification Functions and Average Effective Shear Wave Quality Factor Qseff from Analysis of Accelerograms of the 1999 Chamoli Earthquake, Himalaya
Author/Authors :
Dinesh Kumar، نويسنده , , V. Sri Ram، نويسنده , , K. N. Khattri ، نويسنده ,
Issue Information :
ماهنامه با شماره پیاپی سال 2006
Abstract :
The accelerograms of the 1999 Chamoli earthquake and nine of its aftershocks, which
occurred in Uttaranchal Himalaya, have been analyzed to investigate their source parameters, the site
amplification functions and the average effective shear-wave quality factor Qseff in the region. The fault
plane solution of the main shock is obtained using the spectral amplitudes of SH waves (approximated by
transverse components of accelerograms) of the high-energy packets observed in the accelerograms of the
main shock. It is found to be comparable with the reported solutions in other studies. Similarly the other
source parameters (viz., seismic moment = (5.03±1.7) · 1025 dyne-cm, stress drop = 65 bars, source
duration = 5.2 s and moment magnitude = 6.4) estimated for the main shock are consistent with the
values obtained in other studies. The stress drops estimated for the aftershocks vary from 23 bars to 153
bars and the seismic moment from 1.4 · 1023 dyne-cm to 2.9 · 1023 dyne-cm. The average estimated values
of the effective shear-wave quality factor Qseff vary from 655±359 in the Uttaranchal sector of Himalaya
and 1475±130 in the Delhi region. In general, the Qseff value increases with an increase in the epicentral
distance reflecting the penetration of the waves into deeper layers of the crust as the epicentral distance of
the observation point increases. These values of Qseff indicate that in general the curst is at low
temperatures that will promote brittle behavior and conditions for episodic failure as compared to creep,
under the accumulated strains from plate collision at the Himalaya plate boundary. The site amplification
characteristics at sites have been identified from the frequency bands of significant amplification observed
in the spectral ratios of the horizontal to the vertical component records. The decay of peak ground
acceleration (PGA) values with distance has been investigated using the empirical regression curves vis-a` -
vis the site amplification factors.
Keywords :
quality factor , fault plane solution , accelerogram. , Source parameters , site amplification
Journal title :
Pure and Applied Geophysics
Journal title :
Pure and Applied Geophysics