Proustite occurs in hydrothermal deposits as a phase in the oxidized and supergene zone.
2.
Minerals in the silver-ore veins include polybasite, pyrargyrite, proustite, sphalerite, galena, and tennantite.
3.
In the supergene sulfide enriched zone, ore minerals include pearceite, proustite, tetrahedrite, polybasite, and pyrargyrite.
4.
It is closely allied to, and isomorphous with, the corresponding sulfarsenide known as proustite or light red silver ore.
5.
Depending on the locality it is found accompanied by arsenic, tennantite, proustite, chalcopyrite, galenite, and baryte ( in the type locality ); by kutinaite and paxite ( in Nieder-Beerbach ); or by asenic, bismut, tennantite, loellingite, rammelsbergite, proustite, and quartz ( in Sainte-Marie-aux-Mines ).
6.
Depending on the locality it is found accompanied by arsenic, tennantite, proustite, chalcopyrite, galenite, and baryte ( in the type locality ); by kutinaite and paxite ( in Nieder-Beerbach ); or by asenic, bismut, tennantite, loellingite, rammelsbergite, proustite, and quartz ( in Sainte-Marie-aux-Mines ).
7.
The most common minerals in ore-bearing associations of volcanogenic massive sulfide deposits deposits ( non-metamorphosed or oxidized ) and their modern analogues are pyrite, pyrrhotite, chalcopyrite, covellite, sphalerite, galena, tetrahedrite-tennantite, marcasite, realgar, orpiment, proustite-pyrargyrite, wurtzite, stannite ( carbonates ) quartz and native gold, and are differently distributed in the various associations schematized above.
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