

在售的菱锶矿标本
在售 155 个 · US$60–US$30,000 USD
图库中有 263 个
斯铜碳酸盐/mineral content Strontianite is a carbonate mineral composed of SrCO3. It crystallizes in the orthorhombic system and often forms prismatic, tabular, or blocky crystals with a vitreous to resinous luster and a white to colorless appearance. The mineral commonly occurs as delicate, transparent to translucent crystals that can be euhedrally terminated or intergrown, frequently found in vein and cavity fillings of carbonate rocks. Collectors typically seek clean, well-formed crystals that show sharp faces and clear zoning, especially when contrasting with associated minerals that highlight its crystal form.
- 化学式
- SrCO3
- 稀有度
- Uncommon
- 稳定性
- Stable
- 收藏者关注度
- Moderate Interest
- 分类说明
- Carbonate mineral; Strunz: 5.AA
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查看全部 155 个上架菱锶矿的产地
主要产地
- 奥伯多夫22 个标本
- Minerva No. 1矿14 个标本
- 弗吉尼亚7 个标本
- Wiesergut矿, Oberdorf菱镁矿矿床,Oberdorf an der Laming7 个标本
- 温菲尔德5 个标本
- Neue Hoffnung Gottes矿2 个标本
- 斯特朗申2 个标本
- Denton矿1 个标本
- El Tule市1 个标本
- Maybee采石场1 个标本
关于菱锶矿
Notable specimens come from classic European and North American localities, with historical and current collecting interest centered in environments that host hydrothermal activity and carbonate-rich veins. Countries such as Austria, the UK, Canada, the USA, and Germany have yielded notable crystals, often from mining districts with long-standing mineralogic traditions. Strontianite is valued for its crisp habit, subtle coloration, and the way it complements other carbonate and sulfate associates, making it a staple for cabinet displays and reference collections. It provides a compact, straightforward example of strontium carbonate crystallization and local mineralogical context.






















