Vanadinite Vanadinite Vanadinite is a mineral belonging to the apatite group of phosphates, with the chemical formula Pb(VO)Cl. It is one of the main industrial ores of the metal vanadium and a minor source of lead. A dense, brittle mineral, it is usually found in the form of red hexagonal crystals. It is an uncommon mineral, formed by the oxidation of lead ore deposits such as galena. First discovered in 1801 in Mexico, vanadinite deposits have since been unearthed in South America, Europe, Africa, and North America. Vanadinite is an uncommon mineral, only occurring as the result of chemical alterations to
Mineral Exploration Research Centre deposits, volcanology, geochemistry, and alteration associated with hydrothermal copper-zine-(gold) volcanogenic massive sulfide ore deposits, structure, geochemistry, and alteration associated with hydrothermal orogenic lode gold deposits, mineralogy, geochemistry, and genesis of rare-element and rare-metal pegmatites, and the sedimentology of Mississippi Valley-type (MVT) Pb-Zn deposits and placer Au and U deposits. MERC and the Harquail School of Earth Sciences are a world-leaders in mineral deposits education, offering a Co-Op BSc in Mineral Exploration program, hosting the annual PDAC-sponsored Student-Industry Mineral Exploration Workshop, offering a fully modular ("block") Applied MSc degree in Mineral Exploration, and offering a PhD in Mineral Exploration and Precambrian