{{Infobox mineral
| name = 靛銅礦
| category = 硫化物礦物
| boxwidth =
| boxbgcolor =
| image = Covellite-252597.jpg
| imagesize = 260px
| caption =
| formula = CuS
| IMAsymbol = Cv
| molweight =
| strunz = 2.CA.05a
| dana = 02.08.12.01
| system = 六方
| class = 雙六邊形雙錐體 (6/mmm)
H–M記號：(6/m 2/m 2/m)
| symmetry = P63/mmc
| unit cell = a = 3.7938 Å, c = 16.341 Å; Z = 6
| color = 靛藍色或更深，通常呈高度虹彩，黃銅黃色到深紅色
| habit = 薄片狀晶體和板狀，晶體也呈塊狀到粒狀
| twinning =
| cleavage = {0001}完美
| fracture =
| tenacity = 韌
| mohs = 1.5 - 2
| luster =
半金屬光澤，傾向於樹脂到泥土光澤
| refractive = nω = 1.450 nε = 2.620
| opticalprop = 單軸 (+)
| birefringence =
| pleochroism = 標誌性深藍色到淡藍色
| streak = 鉛灰色
| gravity = 4.6 - 4.8
| melt =
| fusibility = 2.5
| diagnostic =
| solubility =
| diaphaneity = 不透明
| other = 雲母狀解理
| references =
}}
靛銅礦（）是一種稀有的含銅硫化物礦物，化學式為CuS。第一份記錄來自維蘇威火山，它於1832年以N. Covelli的名字正式命名。
参见
- 以人名命名的矿物列表
參考資料
评论 (0)