“…Blue-remaining covellite, C U S~+~, differs from stoichiometric covellite, CuS, in that it appears blue under plane-polarized reflected light, while stoichiometric covellite, blue under unpolarized light, appears red. No occurrences of anilite (Cu,S,), digenite (Cu9S5), or djurleite (Cu,,S,,) were reported, though all are known as products of SRB-induced corrosion (Macdonald et al, 1979;North and MacLeod, 1986;McNeil et al, 1991) and of other sulfiding corrosion under equivalent chemical conditions (Mor and Beccaria, 1975). Baas Becking and Moore (1961) suggest that (metastable) digenite is the first corrosion product, that it then alters to chalcocite, and that this is the only room-temperature wet path from copper or cuprite to chalcocite.…”