Stromeyerite
This article will address the topic of Stromeyerite, which has generated great interest and debate in various circles of society. Stromeyerite has become a reference point in the current discussion, and its relevance is undeniable in the contemporary context. Through a detailed analysis, the different aspects surrounding Stromeyerite will be explored, from its historical origin to its impact today. Its influence in various areas will be examined, as well as the implications it has for different sectors of society. In addition, different perspectives and opinions on Stromeyerite will be presented, with the purpose of offering a holistic and enriching vision on this highly relevant topic.
| Stromeyerite | |
|---|---|
 | |
| General | |
| Category | Sulfide minerals |
| Formula (repeating unit) | AgCuS |
| IMA symbol | Smy[1] |
| Strunz classification | 2.BA.40 |
| Crystal system | Orthorhombic |
| Crystal class | Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) |
| Space group | Cmcm |
Stromeyerite or copper-silver glance[2]: 223 is a sulfide mineral of copper and silver, with the chemical formula AgCuS. It forms opaque blue grey to dark blue orthorhombic crystals.
It was discovered in 1832 in Central Bohemia Region, Czech Republic, and named after the German chemist, Friedrich Stromeyer who performed the first analysis of the mineral.[3][4]
See also
References
- ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- ^ Krivovichev V. G. Mineralogical glossary. Scientific editor A. G. Bulakh. — St.Petersburg: St.Petersburg Univ. Publ. House. 2009. — 556 p. — ISBN 978-5-288-04863-0
- ^ http://www.mindat.org/min-3803.html Mindat
- ^ http://rruff.geo.arizona.edu/doclib/hom/stromeyerite.pdf Mineral Handbook
 | This article about a specific sulfide mineral is a stub. You can help Wikipedia by expanding it. |