簡介:"礦物硫化物及硫鹽銅藍CovelliteSulfides and SulfosaltsThe mineral consists of copper and sulfur and small amounts of iron may be present. Covellite exhibits perfect cleavage in one direction, giving it a sheety, foliated appearance, just like mica sheet, and the thin sheets are flexible.Covellite is a rare and not so well distributed mineral. It is usually found, as secondary origin, with other copper minerals as a coating in zones of sulfide enrichment. Most Covellite minerals are found with other copper sulfides and are therefore more stable.主要由銅和硫所構成,偶而也含有少量的鐵。有一組似雲母般的完全底面解理,可撕裂成極薄的片體,且具有彈性。 銅藍在地表的分布並不多,通常以次生礦物的方式,產在硫化礦床的富集帶內或被覆在其它銅礦的表面上。因多數銅藍是由其它銅礦變化而來,性質較為穩定。"