羟胆矾
成分Cu4〔SO4〕(OH)6。含CuO 70.36%。单斜晶系。晶体呈柱状或针状。集合体呈粒状、块状或肾状。绿至深绿色。玻璃光泽。解理平行｛100｝完全。硬度3.5～4。密度3.97克/厘米3。常见于干旱地区铜矿床的氧化带中。可作为炼铜的矿物原料。
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contributed at 2011-09-29
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Earth System(in Chinese) Mineralogy
Detailed Description
| English |
|---|
| Name | brochantite |
| Chinese |
|---|
| Name | 羟胆矾 |
| Description | 成分Cu4〔SO4〕(OH)6。含CuO 70.36%。单斜晶系。晶体呈柱状或针状。集合体呈粒状、块状或肾状。绿至深绿色。玻璃光泽。解理平行｛100｝完全。硬度3.5～4。密度3.97克/厘米3。常见于干旱地区铜矿床的氧化带中。可作为炼铜的矿物原料。 |
How to Cite
NNU_Group (2011). 羟胆矾, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/a0cada5e-697d-49ca-82de-37b03335a6c6
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