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: Geologists use bornite as an "indicator mineral" to locate copper-rich zones within larger ore systems.
Cu5FeS4cap C u sub 5 cap F e cap S sub 4 ) is a copper iron sulfide mineral famously known as due to its spectacular iridescent tarnish. While fresh surfaces appear metallic copper-red to bronze-brown, exposure to air causes rapid oxidation, resulting in a vibrant, rainbow-like shimmer of purples, blues, and golds. Key Mineralogical Features
: This is the mineral's most striking feature, caused by surface oxidation. However, many commercial "peacock ore" specimens are actually chalcopyrite that has been artificially treated with acid.
: A major ore of copper, typically containing about 63% copper by weight. Physical Properties : Hardness : 3–3.25 on the Mohs scale (relatively soft). Luster : Metallic. Streak : Grayish black.
: It is studied for its unique phase transitions and electrical properties, as it changes structure from orthorhombic to cubic when heated above 228∘C228 raised to the composed with power cap C Aesthetic and Metaphysical Use