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10 DOI: 10.37398/JSR.2021.650102 Abstract: The Precambrian crust of the Aravalli Mountain range mainly comprises several Proterozoic fold belts underlain and determined by rocks of Archaean age like schistgneissgranitic rocks. The remobilization which takes place partly during the Proterozoic orogenesis includes a heterogenous assemblage of biotite gneiss, amphibolite, aluminous paragneiss, quartzite and marble formed during the period 3.5-2.5 Ga. The Banded Gneissic Complex (BGC) having more extensive occurrences in the region is regarded as the oldest supracrustals succession representing some of the primitive sediments composed of unweathered igneous debris overlying the Bundelkhand gneiss. The Aravalli rocks have been subjected to two phases of folding. The Vindhyan rocks occur south of the Aravallis with a faulted contact i.e., Great Boundary Fault, and also with unconformable contact at places. Several evidences have conferred that the fault originated as a thrust and brittle ductile deformation such as en-echelon quartz veins were observed.

Precambrian Evolution and the Deformation Style in the Great Boundary Fault Zone around Chittorgarh, Rajasthan