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12th International Conference & Exposition on Petroleum Geophysics

P- and S-wave velocity modeling and inversion using 3-C seismic data in Western Dharwar Craton (WDC) of southern India to image shallow crustal structure with compositional changes and understand its tectonic settings

Published in GEOHORIZONS - 2017

Deepak Kumar*, Laxmidhar Behera, CSIR-National Geophysical Research Institute, Uppal Road, Hyderabad

Abstract


We present 2-D shallow P- and S-wave velocity models ( and  ) using ray-trace inversion of firstarrival traveltimes picked for the wide-angle 3-C seismic data acquired along the 200 km long E-W trending profile in the Western Dharwar Craton (WDC) of southern India, which traverses across major shear zones like Chitradurga Shear Zone (CSZ). The 2-D velocity models have been constrained to a maximum depth of 15 km mainly confined to the upper crust of this highly complex and oldest (3.2

Keywords


Dharwar Craton; 3-C Seismic data; Modeling; Ray-trace inversion;   ; Poisson

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