Vuoriyarvite-K

vuoriyarvite-K

pyrochlore

strontianite

ewaldite

Images

Formula: (K,Na,☐)12Nb8(Si4O12)4O8.12-16H2O
Cyclosilicate (ring silicate), vuoriyarvite group, labuntsovite supergroup, niobium-bearing mineral
Crystal System: Monoclinic
Specific gravity: 2.95 measured, 3.02 calculated
Hardness: 4½
Streak: White
Colour: White
Luminescence: Not fluorescent
Solubility: Insoluble in dilute hydrochloric and sulphuric acids
Common impurities: Na
Environments

Carbonatites
Hydrothermal environments

Localities

At the type locality, the Vuoriyarvi alkaline-ultrabasic massif, Northern Karelia, Murmansk Oblast, Russia, vuoriyarvite-(K) occurs as dull white tabular crystals up to 3 mm long in veins of dolomite-calcite carbonatite that cut pyroxenites. It formed from hydrothermal alteration of pyrochlore, and is associated with calcite, dolomite, strontianite, ewaldite, serpentine, apatite, pyrrhotite, pyrite, chalcopyrite and sphalerite (AM 83.1347-1352).

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