“…It bisects the Peninsular Indian subcontinent into two halves (Yedekar et al, 1990;Acharyya, 2003). The CITZ lies in the north-northwestern contact formed because of accretion of the Bundelkhand Craton and Bastar Craton (Yedekar et al, 1990;Roy et al, 2001Roy et al, , 2006. The southern boundary of the CITZ is associated with granulite belt with high strain ductile shear zone called Central Indian Suture (CIS) is $500 km in length trending ENE-WSW from southeast of Nagpur to south of Korba (Jain and Yedekar, 1989;Jain et al, 1991;Mall et al, 2008).…”