Pabellóndepicaite
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Cu2+2(N3C2H2)2(NH3)2(NO3)Cl·2H2O
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Pabellóndepicaite is a rare vanadium arsenate mineral first described from the Pabellón de Pica district in northern Chile, one of the world's most mineralogically rich oxidized ore localities. It forms brilliant orange to red microcrystalline masses associated with other vanadate and arsenate minerals in the hyper-arid Chilean desert. The mineral adds to the remarkable diversity of secondary vanadium mineralogy documented from the Atacama Desert region.