红锑矿

{{Infobox mineral
| name = 红锑矿
| category = 氧硫化物
| boxwidth =
| boxbgcolor =
| image = Mineraly.sk - kermezit.jpg
| caption =
| formula = (Sb2S2O)
| molweight =
| strunz = 2.FD.05
| dana = 02.13.01.01
| system = 三斜晶系
| class = Pinacoidal ()
(same H-M symbol)
| symmetry = P
| color = 红色，樱桃红色至紫色
| habit = 针状，纤维状，放射状
| twinning =
| cleavage = {100}完美, {010}不完美
| tenacity = 可剖
| fracture = 易碎
| mohs = 1 - 2
| luster = 金刚石到半金属
| refractive = nα = 2.720 nβ = 2.740 nγ = 2.740
| opticalprop = 双轴 (+)
| birefringence =
| pleochroism = 无
| streak = 棕红
| gravity = 4.5 - 4.8+
| melt =
| fusibility =
| diagnostic =
| solubility =
| diaphaneity = 半透明，不透明
| other =
| references =
}}

红锑矿是一种锑的天然矿物，化学组成为Sb2S2O，是辉锑矿（Sb2S3）不完全氧化的产物。矿石呈樱桃红、深红至黑色。

历史上红锑矿曾被用于做红色颜料，但因其毒性，现已不再使用。

佩济诺克的喀尔巴阡山脉。]]

参考资料

• Bencze, Koloman. “Antimony” pp. 227–235. Handbook on Metals in Clinical and Analytical Chemistry (ed.) Hans G Seiler (1994) ISBN 0-8247-9094-4
• Sneader, Walter. Drug Discovery: A History (2005). ISBN 0-471-89980-1