Frolovite

frolovite

calciborite

olshanskyite

parasibirskite

Images

Formula: Ca[B(OH)4]2
Anhydrous borate containing hydroxyl
Crystal System: Triclinic
Specific gravity: 2.14 to 2.22 measured, 2.259 calculated
Hardness: 3½
Streak: White
Colour: White, with a greyish tint
Luminescence: Luminesces violet in cathode rays (AM 43.385)
Environments

Metamorphic environments
Hydrothermal environments

Frolovite is a rare alteration product of hydrothermal boron minerals in skarn deposits (HOM) in veinlets and irregular masses replacing calciborite (Dana).

Localities

At the Fuka mine, Fuka, Bitchū, Takahashi City, Okayama Prefecture, Japan, frolovite is associated with olshanskyite, parasibirskite, sibirskite, takedaite, pentahydroborite, nifontovite and calcite (HOM).

At the type locality, the Novofrolovskoye B-Cu deposit, Tur'insk, Turya river, Turinsk-Auerbakovsk ore field, Serovsky District, Sverdlovsk Oblast, Russia, frolovite occurs in limestone in the contact-metasomatic copper deposits. It is associated with calciborite, calcite, gypsum, garnet and magnetite, and replaces calciborite (AM 43.385, HOM)

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