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The 3-D shear velocity structure beneath South India&#39;s Dharwar Craton determined from fundamental mode Rayleigh waves phase velocities reveals the existence of anomalously high velocity materials in the depth range of 50–100 km. Tomographic analysis of seismograms recorded on a network of 35 broad-band seismographs shows the uppermost mantle shear wave speeds to be as high as 4.9 kms–1 in the nor...

Complex shallow mantle beneath the Dharwar Craton inferred from Rayleigh wave inversion