Many of the ores of metallic minerals
occur as compounds of the sulfide ion, S2–, with the metals
attached as cations. Most of these are soft and look like metals
and form many of the world’s large ore deposits. One of
the most common sulfide minerals is pyrite, FeS2, found as a
minor component in many rocks and as an accessory mineral
in many ore deposits. Pyrrhotite (Fe7S8–FeS) is a less-common
iron sulfide mineral. Most ore deposits are formed from
hydrothermal fluids. Lead (Pb) and Zinc (Zn) are commonly
found in sulfide compounds such as galena (PbS) and sphalerite
(ZnS), and copper deposits are dominated by the two
sulfide minerals chalcopyrite (CuFeS2) and bornite (Cu5FeS4).
See also MINERALOGY.
sun dogs See SUN HALOS.
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