Br. Prasad et al., STRUCTURE AND TECTONICS OF THE PROTEROZOIC ARAVALLI-DELHI FOLD BELT IN NORTHWESTERN INDIA FROM DEEP SEISMIC-REFLECTION STUDIES, Tectonophysics, 288(1-4), 1998, pp. 31
Seismic imaging of the crust along a 400-km-long deep seismic reflecti
on profile across the Palaeo/Mesoproterozoic Aravalli-Delhi Fold Belt,
in the northwestern Indian Shield, brings into focus its complex stru
cture and provides clues to understand the geological processes involv
ed in the evolution of this belt. The reflectivity pattern varies cons
iderably for different crustal units along the profile. The deep-crust
al reflection data image two sets of oppositely dipping strong reflect
ion bands, from upper-to lower-crustal levels. These are identified as
the signatures of the collision corresponding to Aravalli and Delhi o
rogeny. The data also exhibit a clear Moho and strong lower-crustal re
flections near the collision boundaries. A stack of dipping reflection
s from the top of the Moho to the surface is identified as a major thr
ust fault indicating that the Proterozoic collision and deformation we
re primarily thick-skinned in nature. (C) 1998 Elsevier Science B.V.