ABSTRACT
The host rock for mineralization is Graphitemicasillimanite Gneiss/Schist (GMS) and consists of mica (white, green and brown varieties), feldspar, quartz and an appreciable amount of graphite.
Walls are composed of Garnet Biotite Sillemanite Gneiss (GBSG) and intrusions of Pegmatite and Amphibolite and Mylonite (on footwall only) while GBSG forms the major chunk amounting around 70-80% of the mass.
