白碲金银矿

{{Infobox mineral
| name = 白碲金银矿
| category = 碲化物矿物
| boxwidth =
| boxbgcolor =
| image = Krennerite-118303.jpg
| imagesize = 260px
| caption = Krennerite in a quartz vein, Cresson Mine, Cripple Creek, Colorado
| formula = AuTe2 to Au3AgTe8
| molweight =
| strunz = 2.EA.15
| system = Orthorhombic
| class = Pyramidal (mm2)
| symmetry = Orthorhombic
H-M记号: (mm2)
空间群: Pma2
| color = 银白色至黄铜色，或乳白色（抛光）
| habit = Massive to crystalline with short striated prismatic crystals
| twinning =
| cleavage = Perfect on {001}
| fracture = Subconchoidal - uneven
| tenacity = Brittle
| mohs = 2.5
| luster = 高度金属性
| polish =
| refractive = Opaque
| opticalprop = Anisotrophism strong
| birefringence =
| dispersion =
| pleochroism = weak
| fluorescence= None
| absorption =
| streak = 绿灰色
| gravity = 8.62
| density =
| melt =
| fusibility =
| diagnostic =
| solubility =
| diaphaneity = opaque
| other =
| references =
}}
白碲金银矿（英语：Krennerite）是一种正交的碲化金矿物，该矿物中可能含有一定量的银，其结构式为Au1-xAgxTe2（x=0−0.2）。其它金银碲化物矿物，如和针碲金银矿是单斜晶系的，而白碲金银矿是正交晶系的。
参考文献