Manoj Pandit
Department of Geology, University of Rajasthan, Jaipur - 302004, Rajasthan, India
[ 1 ] - Recurrent seismicity in Rajasthan State in the tectonically stable NW Indian Craton
Indian peninsular region comprises several Archean cratonic blocks (Dharwar, Bastar, Singhbhum, Aravalli – Bundelkhand), bordered by Proterozoic mobile belts. Therefore, this region is considered as tectonically stable and designated as the least vulnerable region to earthquake hazard except the still active Central Indian Tectonic Zone (CITZ). The latter is a major suture between southern and ...
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