Parasterryite

parasterryite

sterryite

famatinite

geocronite

Images

Formula: Ag4Pb20(Sb,As)24S58
Sulphosalt, antimony- and arsenic- bearing mineral
Crystal System: Monoclinic
Specific gravity: 5.747 calculated for the ideal formula
Hardness: 3 to 3½
Streak: Black
Colour: Black
Environments

Metamorphic environments
Hydrothermal environments

Parasterryite is a relatively new mineral, approved in 2010 and to date (July 2024) reported only from the type locality.

Localities

The type locality, the Pollone Mine, Valdicastello Carducci, Pietrasanta, Lucca Province, Tuscany, Italy, was exploited in the Middle Ages for silver-bearing galena, and in the 20th century for baryte.
In 2010 parasterryite and sterryite were collected independently in vugs within barytequartz veins embedded in barytepyrite lenses. An overgrowth of minute yellow-green crystals of sphalerite was observed on the sterryite needles, but parasterryite is free of any sulphide or sulphosalt. Acanthite, famatinite, geocronitejordanite, pyrargyriteproustite, antimony-rich rathite, tetrahedrite and xanthoconite were also identified in the same occurrence. Owyheeite and a boulangerite-like sulphosalt have been found in this kind of occurrence, but they were not identified in the samples studied. Boulangerite was identified in quartz veins embedded in the country rocks, as acicular to prismatic crystals, up to several cm in length.
Parasterryite occurs as metallic black needles striated along their elongation, up to several mm in length and 0.2 to 0.3 mm thick (CM 49.2.623-638).

Back to Minerals