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The Indian plate has a unique history of evolution subsequent to its separation from the Gondwana supercontinent. At present, it is a collage of complex structural terranes of varied geology, ranging from collision, subduction, paleo rifts, mobile belts, cratons and basins (Fig. 1). During the past five years, several seismological studies have been undertaken at various geological terrains by many organisations and individuals to decipher the crustal architecture, seismotectonics, geodynomics and earthquake occurrence processes in the plate boundary as well as in the plate interiors. Significant efforts have been made to estimate the source parameters (both dynamic and static) of the earthquakes which have occurred in the Indian subcontinent. GPS measurements have been made at a number of sites to determine the convergence rate, strain budget and role of various tectonic units in accommodating the plate motion. A major initiative was taken up by the Ministry of Earth Sciences to upgrade and upscale the national seismological network. We have restricted this review to some significant work done by the Indians on the Indian landmass. We do not claim that this is an exhaustive review, and any omissions are unintentional. Crustal Architecture of the Indian Subcontinent

A review of seismological research in India during the past five years (2015-2019)