Fleischerite
| Fleischerite | |
|---|---|
| General | |
| Category | Sulfate mineral |
| Formula (repeating unit) | Pb3Ge(SO4)2(OH)6 · 3H2O |
| IMA symbol | fsh |
| Strunz classification | 7.DF.25 |
| Dana classification | 31.07.06.03 (hydrated silicates containing hydroxyl or halogen) |
| Crystal system | Hexagonal |
| Identification | |
| Color | White, light reddish-pink |
| Crystal habit | Accicular |
| Tenacity | brittle |
| Mohs scale hardness | 2.5-3 |
| Luster | Sub-vitreous, silky |
| Streak | White |
| Density | 4.3 |
| Birefringence | 0.029 |
| Pleochroism | Non-pleochroic |
Fleischerite is a type of mineral. Named after Michael Fleischer, a co-founder of the International Mineralogical Association.[1] Recognized in 1960. Has its own group made of itself, schaurteite, despujolsite, mallestigite, and genplesite.[2] It is often confused with dundasite.
Occurence
[edit]Fleischerite is found only in Tsumeb (Ongopolo) Mine, Namibia. It forms in oxidized portions of a dolostone-hosted hydrothermal germanium-bearing polymetallic ore deposits.[3] The oldest samples are estimated to be 541 million years old.[4]