Girvasite

girvasite

bobierrite

pyrite

dolomite

Images

Formula: NaCa2Mg3(PO4)3(CO3)(H2O)6
Compound phosphate
Specific gravity: 2.46 measured, 2.529 calculated
Hardness: 3½
Streak: White
Colour: Creamy white, colourless
Luminescence: Not fluorescent under UV
Solubility: Readily soluble in cold 10% hydrochloric acid
Environments

Carbonatites
Hydrothermal environments

Localities

At the type locality, the Kovdor Zheleznyi mine, Kovdor Massif, Murmansk Oblast, Russia, girvasite forms creamy white spherulites to 1.5 mm in diameter, and rarely colourless and transparent single prismatic crystals up to 1 mm long and 0.07 mm across. It occurs in solution cavities in dolomite carbonatite intimately intergrown with bobierrite; minor pyrite is also present, and dolomite lines the cavities. Girvasite is a low-temperature, hydrothermal mineral formed from phosphatic solutions at 100 to 250oC (AM 77.207).

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