Teleseismic earthquake waveform data from 10 broadband stations spread over
the Indian shield and in operation since 1997, were analyzed to infer the
crustal structure, using the receiver function technique. The South Indian
shield is characterized by a 33-39 km thick, and remarkably simple crust, w
ith an average Poisson's ratio close to 0.25. The Archaean crust is devoid
of any prominent intra-crustal discontinuities. The velocity contrast at th
e well developed Moho is large, resulting in very clear P-to-S conversions
as well as first-order multiples. In contrast, the predominantly Proterozoi
c crust in the northern part of the shield exhibits a complex character, du
e to the presence of additional seismic discontinuities. Moho conversions,
which are considerably weaker compared to the Archaean terrains, indicate c
rustal thicknesses of more than 40 km.