Argentopyrite is a moderately rare sulfide mineral with the chemical formula . It is one of the natural compounds of the type, with M being caesium in very rare pautovite, copper in relatively common cubanite, potassium in rare rasvumite and thallium in rare picotpaulite. The type locality is Jáchymov in Czech Republic. Chemically similar mineral include sternbergite (dimorphous with argentopyrite), lenaite, , and argentopentlandite, .
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Argentopyrite is a moderately rare sulfide mineral with the chemical formula . It is one of the natural compounds of the type, with M being caesium in very rare pautovite, copper in relatively common cubanite, potassium in rare rasvumite and thallium in rare picotpaulite. The type locality is Jáchymov in Czech Republic. Chemically similar mineral include sternbergite (dimorphous with argentopyrite), lenaite, , and argentopentlandite, .
==Crystal structure== Although previously assumed orthorhombic, argentopyrite was later shown to be monoclinic, with structural relationship to cubanite. The most important feature of the argentopyrite structure are: hexagonal close-packing of sulfur atoms presence of and tetrahedra in sheets displaying corner-sharing presence of a cluster of four tetrahedra that share edges presence of two iron sites, instead of one as in related species ordered-disordered ferrous-ferric nature of the mineral
Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).