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Crustal Velocity Structure of the Indian Shield from Deep Seismic Sounding and Receiver Function Studies
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The average crustal velocity and Moho depth, estimated from the data of more than 5000 km deep seismic sounding (DSS) profiles and a number of broadband seismological stations covering various geological and tectonic units of the Indian shield have been presented. The average crustal velocity varies from 62 to 65 km/s except at few anomalous regions. The average crustal thickness varies from 40 to 42 km except in Dharwar craton (35-45 km) and southernmost part of the southern granulite terrain (35-38 km). The crust is thinner towards both eastern and western coasts of the shield. The crust to the north of the west coast is again thinner (-25 km) than that of the east coast (-35-37 km) with a prominent up-Warp at the eastern flank of the West-Bengal Basin (-30-32 km). The shallowing of the crust towards the coast is due to underplating and breakup of the Indian shield from the Gondwanaland.
Keywords
DSS, Broadband Seismology, Moho, Crustal Structure, Indian Shield.
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