Chalcopyrite ore deposit. Chalcopyrite Group. Named in 1725 by Johann Friedrich Henckel from the Greek "chalkos", copper, and "pyrites", strike fire. Common in sulfide veins and disseminated in igneous rocks. Chalcopyrite is present with many ore-bearing environments via a variety of ore forming processes. Because of its abundance and ease of extraction, chalcopyrite is the dominant ore for obtaining copper. Chalcopyrite-Eskebornite Series. Chalcopyrite is a copper iron sulfide mineral, with the chemical formula CuFeSâ‚‚. It was named from the Greek word for “Copper” and “Brass”, and can most notably be seen as shades of yellow, green and grey. A major ore of copper. It occurs in most sulfide mineral deposits throughout the world and has been the most important ore of copper for thousands of years. Comments: White moncheite with chalcopyrite (orange, blue and violet tarnishing colors) in silicate matrix. Chalcopyrite is present with many ore-bearing environments via a variety of ore forming processes. Polished section (from microprobe analysis) in reflected light. Chalcopyrite is a Copper iron sulfide mineral that was first found in 1725 by J. Chalcopyrite is a striking, bright yellow, metallic mineral that occurs in nearly all sulfide deposits. Initially, it may be easy to confuse chalcopyrite, or copper pyrite (CuFeS2), with pyrite (FeS2), but the two can be distinguished by their relative hardness and chalcopyrite’s iridescent tarnish. Chalcopyrite is a brass-yellow mineral with a chemical composition of CuFeS 2. F Henckel. . Chalcopyrite is present in volcanogenic massive sulfide ore deposits and sedimentary exhalative deposits, formed by deposition of copper during hydrothermal circulation. tusgqhllwpfd0vzb71mlsvhnywbac53o2w0bli