| 词条 | Renierite |
| 释义 |
| name = Renierite | category = Sulfide mineral | boxwidth = | boxbgcolor = | image = Renierit.JPG | imagesize = | caption = | formula = (Cu,Zn)11(Ge,As)2Fe4S16 | molweight = | strunz = 2.CB.35a | system = Tetragonal | class = Scalenohedral ({{overline|4}}2m) H-M symbol: ({{overline|4}} 2m) | symmetry = P{{overline|4}}2c | color = bronze yellow, pinkish brown | habit = granular | twinning = | cleavage = absent | fracture = Uneven | mohs = 4.5 | luster = metallic | refractive = opaque | opticalprop = | birefringence = | pleochroism = | streak = dark gray | gravity = 4.4 | density = | melt = | fusibility = | diagnostic = | solubility = | diaphaneity = | other = }} Renierite, (Cu,Zn)11(Ge,As)2Fe4S16 is a rare copper zinc germanium bearing sulfide mineral. It occurs at the Kipushi Mine, Democratic Republic of the Congo; and Namibia, among other places. Renierite was named after Armand Renier (26 June 1876 - 9 October 1951), a Belgian geologist and Director of the Belgian Geological Survey.[1][2] References1. ^Webmineral {{Sulfide-mineral-stub}}2. ^Mindat 4 : Zinc minerals|Sulfide minerals|Germanium minerals|Tetragonal minerals |
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