赤铜矿
成分Cu2O，含Cu 88.8%。等轴晶系。晶体呈细小八面体，有时呈针状或毛发状称为针赤铜矿；集合体呈粒状、致密块状或土状。暗红色。条痕褐红色。金刚光泽或半金属光泽。硬度3.5～4。密度6克/厘米3。形成于外生条件下，主要见于铜矿床氧化带，是含铜硫化物氧化后的产物。可作为铜矿石利用。
Classification(s)
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Geographic semantic resource library Earth System(in Chinese) Mineralogy
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| English |
|---|
| Name | cuprite |
| Chinese |
|---|
| Name | 赤铜矿 |
| Description | 成分Cu2O，含Cu 88.8%。等轴晶系。晶体呈细小八面体，有时呈针状或毛发状称为针赤铜矿；集合体呈粒状、致密块状或土状。暗红色。条痕褐红色。金刚光泽或半金属光泽。硬度3.5～4。密度6克/厘米3。形成于外生条件下，主要见于铜矿床氧化带，是含铜硫化物氧化后的产物。可作为铜矿石利用。 |
{{htmlJSON.HowtoCite}}
NNU_Group (2011). 赤铜矿, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/ca021d21-bfb8-43ba-b83f-e82f6587f264
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