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Published August 2004 | Published
Journal Article Open

A Source Study of the Bhuj, India, Earthquake of 26 January 2001 (M_w 7.6)

Abstract

We study the source time function (STF) and radiated seismic energy (E_R) of the M_w 7.6 Bhuj earthquake using the empirical Green's function (EGF) technique. Our estimations of the STF and E_R are based on teleseismic P waves and regional seismograms, respectively. We find that the STFs as a function of azimuth have a similar shape and nearly constant duration of 18 sec. This suggests that the rupture propagation was essentially radial. The STFs show a sharp rise in the first 6 sec. The E_R estimated from the EGF technique is 2.1 × 10^(23) erg. We find that E_R's computed from integration of corrected velocity-squared spectra of teleseismic P waves and regional seismograms are in excellent agreement with the ER obtained from the EGF technique. Since the seismic moment, M_0, is 3.4 × 10^(27) dyne cm, we obtain E_R/M_0 = 6.2 × 10^(-5). The radiation efficiency, η_R, during the Bhuj earthquake was low, about 0.23. The sharp rise of the STFs and η_R = 0.23 can be explained by Sato and Hirasawa's (1973) quasi-dynamic, circular source model with an effective stress of ∼ 300 bar and the ratio of rupture to shear-wave velocity, V_R/β, of ∼ 0.5. The corresponding estimate of slip velocity at the center of the fault is 156 cm/sec. V_R/β ∼ 0.5 is in reasonable agreement with the duration of the STF and the reported dimension of the aftershocks, as well as with the results of inversion of teleseismic body waves. The observations may also be explained by a frictional sliding model, with gradual frictional stress drop and significant dissipation of energy on the fault plane. This model requires an average dynamic stress drop of about 120 bar and V_R/β ∼ 0.7 to explain both the rapid rise in the first 6 sec of the STFs and, along with a static stress drop of 200 bar, the observed E_R/M_0. High static stress drop is a common feature of most crustal earthquakes in stable continental regions. An examination of the available data, however, does not suggest that most of them also have relatively low radiation efficiency.

Additional Information

© 2004 Seismological Society of America. Manuscript received 10 October 2003. We express our gratitude to the authorities of the following institutions in India for making data available: India Meteorological Department/ Department of Science and Technology; DEQ, I.I.T., Roorkee; National Geophysical Research Institute; Geological Survey of India; Gujrat Engineering Research Institute; Osmania University; Indian Institute of Geomagnetism, Mumbai; Wadia Institute of Himalyan Geology; Centre for Earth Science Studies; and National Institute of Rock Mechanics. We are grateful to the Director General of India Meteorological Department for permission to use the data. We thank the Secretary, DST, for his continuous support. A preliminary version of the manuscript was revised by Jack Boatwright. We thank Hiroo Kanamori, Tamao Sato, and the associate editor for their incisive comments. The research was partially supported by UNAM, DGAPA Projects IN111601.

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Created:
August 19, 2023
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October 26, 2023