Chalcocite is sometimes found as a primary vein mineral in hydrothermal veins.
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Common copper minerals are chalcopyrite and chalcocite.
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However, a chalcocite-enriched zone occurs below the oxidation zone on the south side of the Creston Main Zone.
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The transition zone is composed of chalcocite and bornite with malachite on fractures and a minor amount of chalcopyrite.
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The term chalcocite comes from the alteration of the obsolete name chalcosine, from the Greekkhalkos, meaning copper.
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Chalcocite concentrates typically grade between 37% and 40% copper-in-concentrate, as chalcocite has no iron within the mineral.
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If the results indicate good recovery of the chalcocite and bornite, the transition zone might be added to the evaluation of the oxide material.
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Chalcocite has been known to form pseudomorphs of the minerals bornite, covellite, chalcopyrite, pyrite, enargite, millerite, galena and sphalerite.
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However, most chalcocite occurs in the supergene enriched environment below the oxidation zone of copper deposits as a result of the leaching of copper from the oxidized minerals.
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More examples
A heavy grey mineral that is an ore of copper
Chalcocite, copper(I) sulfide (Cu2S), is an important copper ore mineral. It is opaque and dark-gray to black with a metallic luster. It has a hardness of 2u00BD - 3 on the Mohs scale. It is a sulfide with an orthorhombic crystal system.
Cuprous sulphide, Cu2S, an important ore of copper
A sulphide mineral of copper common in the zone of secondary enrichment.