Mineral Compositions of the Charnockitic Rocks from Kondapalli and Correlations with the Whole Rock Compositions

This communication is aimed at evaluating the compositional relationships between the minerals and host charnockitic rocks from Kondapalli and to demonstrate that the composition of any particular ferromagnesian mineral in the granulites is controlled not by the whole rock chemistry alone but by the amount and actual composition of all other coexisting ferromagnesian minerals and also of the ore minerals.