“…The evolution of the Indian Ocean, the present morphology and tectonics of the bordering continental margins are the consequences of the breakup of Eastern Gondwana land and subsequent seafloor spreading between the constituent continents viz., Madagascar, Seychelles, India, Antarctica, and Australia, since the Early Cretaceous (Murthy et al, 2011). The recent occurrence of earthquakes in coastal regions of the East as well as West Coasts of India has invoked interest among the earth scientists to study the coastal seismicity in relation to morphological and tectonic lineaments associated with coastal and near-shore regions of the continental shelf (Murthy et al, 2010).…”