Ferrimuirite
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Ba10(Ca2Fe3+2)[Si8O24]O2Cl10
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Ferrimuirite is a rare iron-dominant analogue of muirite, a complex barium titanium silicate mineral found in alkaline igneous rocks and associated metasomatic zones. It occurs as brown to dark brownish-red prismatic crystals with a subadamantine luster. The mineral contributes to understanding Fe-Ba-Ti silicate chemistry in alkaline magmatic and metasomatic environments.