STIBICONITE. Catorce, San Luis Potosí, Mexiko (großes Kabinettstück)
Stibiconit ist ein seltenes Mineral, das aus Antimonoxid besteht und die Formel Sb3O6(OH) hat. Der Name leitet sich von den griechischen Wörtern stíbi (στίβι), was „Antimon“ bedeutet, und kónis (κόνις), was „Pulver“ bedeutet, ab und spiegelt seine chemische Zusammensetzung und physikalische Form wider. Dieses Mineral gehört zur Pyrochlor-Supergruppe.
Erstmals 1862 an einem Fundort im Distrikt Brandholz – Goldkronach des Fichtelgebirges in Bayern, Deutschland, identifiziert, bildet sich Stibiconit als sekundäres Alterationsprodukt hydrothermaler Antimonminerale, insbesondere Stibnit. Es wird typischerweise zusammen mit anderen Mineralien wie Cervantit, Valentinit, Kermesit, gediegenem Antimon und Stibnit gefunden.
PSEUDOMORPHOSE NACH STILBIT
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