Burckhardtite

burckhardtite

dickite

moctezumite

zemannite

Images

Formula: Pb2(Fe3+Te6+)(AlSi3O8)O6
Unclassified silicate, tellurium-bearing mineral
Crystal System: Trigonal
Specific gravity: 4.96 calculated
Hardness: 2
Streak: Pale red
Colour: Carmine-red to violet-red, pink, brown
Solubility: Insoluble in hot dilute or concentrated HCl.
Magnetism: Paramagnetic
Environments

Sedimentary environments
Hydrothermal environments

Localities

At the type locality, the Moctezuma mine, Moctezuma, Moctezuma Municipality, Sonora, Mexico, burckhardtite is relatively common on the third level, where it occurs in extremely thin disseminations on angular fragments of light grey cryptocrystalline quartz in a breccia loosely cemented by dickite. Associated minerals are moctezumite and less commonly zemannite and baryte. Burckhardtite forms minute rosettes of carminered crystals about 0.l mm in size. The rosettes are tightly attached to the quartz, and can be removed only by scraping, which tends to break up the crystals.
On the second level of the mine some burckhardtite was found in small open fractures, associated with dickite, zemannite, moctezumite and tellurite. Here the burckhardtite formed larger rosettes, up to 0.3 mm, with occasional single crystals 50 microns across. Most of the crystalline rosettes have centres of dickite, suggesting an oriented overgrowth (AM 64.355-358).

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