硒铅矿

{{Infobox mineral
| name = 硒铅矿
| category = 硒化物矿物
| boxwidth =
| image = Clausthalite-207330.jpg
| imagesize = 260px
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| formula = PbSe
| IMAsymbol = Cth
| molweight =
| strunz = 2.CD.10
| dana = 02.08.01.02
| system = 立方晶系
| class = -{zh-tw:六八面晶族; zh-cn:六八面体;}- (mm)
H-M記號: (4/m 2/m)
| symmetry = Fmm
| color = 蓝灰色至铅灰色
| habit = 致密到颗粒状，有自形晶
| twinning =
| cleavage = {001}良好解理
| fracture = 不規則/參差斷口
| tenacity = 脆性
| mohs = 2.5 - 3
| luster = 金属光泽
| streak = 灰黑色
| diaphaneity = 不透明
| gravity = 7.6 - 8.8
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}}
硒铅矿（）是一种含铅的硒化物矿物，化学式为PbSe。它与方铅矿（PbS）形成固溶体。

产生
硒铅矿發現於含有其他硒化物的低硫热液矿床和汞矿床中。常共生硒汞矿、蓝硒铜矿、硒铜矿、红硒铜矿、金、锑钯矿和晶质铀矿。

它于1832年首次被描述，并以发现地德国哈茨山的克劳斯塔尔-采勒费尔德命名。

参考资料