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The IOG rocks formed prolific mineralization of Fe, Mn, Cr, Ti, Cu, Ni, Au and platinum group elements(PGE). The metamorphosed mafic-ultramafic rocks are mainly schistose and banded amphibolites.
Multiple phases of tectonism and partial melting of crustal materials ultimately led to the formation of Singhbhun Granite Type-B (Phase-III) around 3100 Ma which later intruded the folded and metamorphosed IOG rocks. Saha  based on mineralogy and geochemistry, considered that the schistose amphibolite , hornblende schist and some massive varieties are formed from magmatic rocks (ortho-amphibolite), whereas the banded amphibolites are formed by metamorphism of calc-magnesian sediments (para-amphibolite).
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