S. Farooq et N. Hasan, SULFIDE MINERALIZATION IN THE PARSOI FORMATION OF MAHAKOSHAL GROUP, SOUTHERN MIRZAPUR DISTRICT, UP, Journal of the Geological Society of India, 47(6), 1996, pp. 675-682
Surface indications of sulphide mineralization were noticed in the for
m of gossan bands outcropping as cellular, spongy and boxwork structur
es of limonite in the marble of Parsoi Formation of Mahakoshal Belt ne
ar Ningha village in southern Mirzapur district. Investigations reveal
that mineralization is localized along fractures, shears and zones of
brecciation in the marble, and is controlled by the structural patter
ns of the host rocks. Sulphide mineral assemblage consists of pyrite,
pyrrhotite, cobaltite, chalcopyrite, sphalerite, galena, proustite and
pyrargyrite. The sulphides are found to occur in the form of veins, s
tringers and disseminations. Mineralogical assemblages and textural ch
aracteristics of the altered and sulphide zones indicate that minerali
zation is hypothermal in nature.