Publication | Open Access
Seismic imaging of the aftershock zone of the 2001 <i>Mw</i> 7.7 Bhuj earthquake, India
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Citations
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References
2006
Year
Mw 7.7EngineeringSeismic WaveEarthquake HazardsBhuj EarthquakeActive TectonicsEarth ScienceGeophysicsAftershock ZoneEarthquake SourceRegional TectonicsBanni BasinNeotectonicsMarine GeologyGeographySeismic ImagingGeologyEarthquake RuptureTectonicsSeismologySubduction ZoneCivil EngineeringSeismic Hazard
Detailed seismic tomography reveals that the 2001 Mw 7.7 Bhuj earthquake was associated with a 10–14% increase in Vp and Vs and a 10% decrease in Vp/Vs in the 10 to 35 km depth range covering a 2750 km 2 area beneath the aftershock zone. This anomaly could be attributed to the existence of a lithological heterogeneity or a pluton of mafic composition that might have intruded during the rifting in early Jurassic (∼160 Ma). The Banni basin and the Wagad uplift are found to be associated with high velocity intrusive bodies extending from 5 to 35 km depth. A few patches of low Vp and Vs and high Vp/Vs between 10 to 30 km depth have also been detected on the causative 45° south dipping north Wagad fault (NWF) for the 2001 mainshock, which may be attributed to a fluid filled fractured rock matrix.
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