 | This article needs additional citations for
verification. (February 2022) |
| Geocronite | |
|---|---|
 | |
| General | |
| Category | Sulfosalt minerals |
|
Formula (repeating unit) | Pb14(Sb, As)6S23 |
| IMA symbol | Geo [1] |
| Strunz classification | 2.JB.30a |
| Crystal system | Monoclinic |
| Crystal class | Prismatic (2/m) (same H-M symbol) |
| Space group | P21/m |
Geocronite is a mineral, a mixed sulfosalt containing lead, antimony, and arsenic with a formula of Pb14(Sb, As)6S23. Geocronite is the antimony-rich endmember of a solid solution series. The arsenic-rich endmember is named jordanite. It occurs as grey, black, to silvery white monoclinic crystals. It is found in hydrothermal veins usually associated with other similar minerals, particularly the sulfides of iron and copper.
The mineral has been found in Spain, Ireland and Sweden where it was first identified in 1839.
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.
External links
 | This article about a specific sulfide mineral is a stub. You can help Wikipedia by expanding it. |
| This article needs additional citations for
verification. (February 2022) |
| Geocronite | |
|---|---|
|
| |
| General | |
| Category | Sulfosalt minerals |
|
Formula (repeating unit) | Pb14(Sb, As)6S23 |
| IMA symbol | Geo [1] |
| Strunz classification | 2.JB.30a |
| Crystal system | Monoclinic |
| Crystal class | Prismatic (2/m) (same H-M symbol) |
| Space group | P21/m |
Geocronite is a mineral, a mixed sulfosalt containing lead, antimony, and arsenic with a formula of Pb14(Sb, As)6S23. Geocronite is the antimony-rich endmember of a solid solution series. The arsenic-rich endmember is named jordanite. It occurs as grey, black, to silvery white monoclinic crystals. It is found in hydrothermal veins usually associated with other similar minerals, particularly the sulfides of iron and copper.
The mineral has been found in Spain, Ireland and Sweden where it was first identified in 1839.
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.
External links
|
| This article about a specific sulfide mineral is a stub. You can help Wikipedia by expanding it. |