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.

Fleischerite
General
CategorySulfate mineral
Formula
(repeating unit)
Pb3Ge(SO4)2(OH)6 · 3H2O
IMA symbolfsh
Strunz classification7.DF.25
Dana classification31.07.06.03 (hydrated silicates containing hydroxyl or halogen)
Crystal systemHexagonal
Identification
ColorWhite, light reddish-pink
Crystal habitAccicular
Tenacitybrittle
Mohs scale hardness2.5-3
LusterSub-vitreous, silky
StreakWhite
Density4.3
Birefringence0.029
PleochroismNon-pleochroic

Occurrence

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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]

References

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  1. ^ "Fleischerite". mindat.org. Retrieved 2024-11-14.
  2. ^ "The Fleischerite Group of Minerals | Fred Haynes". 2016-12-14. Retrieved 2024-11-14.
  3. ^ "Fleischerite Mineral Data". webmineral.com. Retrieved 2024-11-14.
  4. ^ "Dynamic Earth Collection - About". dynamicearthcollection.com. Retrieved 2024-11-14.