磷铝锂石
成分LiAl〔PO4〕(F，OH)。三斜晶系。晶体呈等轴状，通常呈细粒状或放射状集合体。白色、乳白色、蓝白色。玻璃光泽。解理面呈珍珠光泽。硬度5.5～6。解理平行｛100｝完全，平行｛110｝中等。密度3.11克/厘米3。是富锂伟晶岩的典型矿物。是提取锂的矿物原料。
53
Alias
Contributor
contributed at 2011-09-29
Classification(s)
●
Earth System(in Chinese) Mineralogy
Detailed Description
| English |
|---|
| Name | amblygonite |
| Chinese |
|---|
| Name | 磷铝锂石 |
| Description | 成分LiAl〔PO4〕(F，OH)。三斜晶系。晶体呈等轴状，通常呈细粒状或放射状集合体。白色、乳白色、蓝白色。玻璃光泽。解理面呈珍珠光泽。硬度5.5～6。解理平行｛100｝完全，平行｛110｝中等。密度3.11克/厘米3。是富锂伟晶岩的典型矿物。是提取锂的矿物原料。 |
How to Cite
NNU_Group (2011). 磷铝锂石, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/cf4422ae-539c-48ac-8031-5d31ba226eba
Copy
Copyright and Disclaimer
All copyrights of a material (model, data, article, etc.) in the OpenGMS fully belong to its author/developer/designer (or any other wording about the owner). The OpenGMS takes every care to avoid copyright infringement, contributor(s) should carefully employ materials from other sources and give proper citations.
