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The shear velocity structure of the north Indian crust comprising of the Archean cratons (Aravalli–Bundelkhand) and Proterozoic Vindhyan basin is modeled and compared with the eastern Dharwar craton as well the global models for Archean and Proterozoic terrains. The velocity structure is deduced from joint inversion of teleseismic receiver function time series and surface wave group velocity measurements...
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