Journal of Geological Society of India (Online archive from Vol 1 to Vol 78)

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The green garnets found in the calc-silicate horizons around Bandihalli, is a chrome grossular (∼7% Cr2O3) with appreciable amount of Mn content. Thus, a partial miscibility between uvarovite and spessartite end members appears possible. The occurrence of thin band of graphite bearing quartzite within the calc-silicate horizons points to its metasedimentary origin. The presence of another variety of garnet (pyrope-almandine rich) in the associated cordierite bearing rock of the area shows that the composition of garnet may not be wholly dependant on grade of metamorphism.
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