PHLOGOPITE

also called brown mica basic aluminosilicate of potassium, magnesium, and iron that is a member of the common mica group. Varieties that contain only small amounts of iron are economically important as electrical insulators. Phlogopite occurs typically as a metamorphic product (e.g., in crystalline metamorphosed limestones) and also in ultrabasic igneous rocks. Phlogopite forms a chemical substitution series with biotite, from which it is arbitrarily distinguished by a magnesium-to-iron ratio greater than 2:1. For detailed physical properties, see mica (table). The name phlogopite also denotes an iron-free compound regarded as making up a large part of the mineral. Its chemical composition is K2Mg6(Si6Al2O20)(OH)4.