Cahnite

cahnite

willemite

phillipsite

chabazite

Images

Formula: Ca2B(AsO4)(OH)4
Compound arsenate
Crystal System: Tetragonal
Specific gravity: 3.156
Hardness: 3
Streak: White
Colour: Colorless to white, also golden brown; colourless in transmitted light.
Solubility: Readily soluble in dilute hydrochloric acid
Environments:

Pegmatites
Metamorphic environments

Cahnite is a rare arsenate.

Localities

At the Shijiang Shan-Shalonggou mining area, Inner Mongolia, China, the mineral deposits occur predominantly in veins of hydrothermal origin in skarn. Cahnite was first found here in association with borcarite as pseudotetrahedral crystals in groups adhering to the surfaces of much larger borcarite crystal clusters. The cahnite crystals are greyish white and up to about 2 mm. Later finds were of pseudotetrahedral crystals of cahnite associated with olshanskyite, johnbaumite or roweite but not with borcarite. The crystals of cahnite are white and opaque, to 3 mm, and have faces that are rough and uneven (R&M 96.5.400).
Cahnite from Shijiang Shan - Image

At Capo di Bove, Italy, cahnite occurs with zeolites in leucitic lava associated with phillipsite, chabazite and calcite (HOM).

At Charcas, Charcas Municipality, San Luis Potosí, Mexico, the primary minerals are sphalerite, galena, chalcopyrite, bornite, tetrahedrite, arsenopyrite, pyrite and silver minerals such as jalpaite, diaphorite and acanthite. In the host rock, as metamorphic or alteration minerals, danburite, datolite, hedenbergite, epidote, chlorite, andradite, actinolite and wollastonite have been reported.
Quartz, calcite and danburite crystallised during the entire life of the systems, throughout the intrusive emplacement, metamorphism, and mineralising events. With depth, both sphalerite and galena decrease while chalcopyrite increases.
Secondary sulphides formed include bornite, covellite, digenite and chalcocite. Native silver, native gold, hematite and goethite were deposited after the sulphides (Minrec 55.6.727-728).
Cahnite crystals range from less than a 1 mm to 2 mm on rare occasions. It occurs as beige sphenoids associated with borcarite and calcite. Based on current (2024) knowledge, less than 10% of the borcarite specimens have cahnite associated with them (Minrec 55.6.737).

At the Kombat mine, Namibia, cahnite is associated with natronambulite, gypsum, baryte and calcite (HOM).
Cahnite from the Kombat Mine - Image

In Siberia, Russia, cahnite is associated with svabite, magnetite, sphalerite, garnet and calcite (HOM).

At the type locality, the Franklin Mine, New Jersey, USA, cahnite is a late-stage mineral in pegmatites cutting a metamorphosed stratiform zinc orebody, associated with hedyphane, friedelite, pyrochroite, franklinite, willemite, rhodonite, datolite, axinite, jarosewichite, samfowlerite, flinkite, hodgkinsonite, hetaerolite, hausmannite, groutite, kentrolite, garnet and baryte (HOM , Mindat).
Cahnite from the Franklin Mine - Image

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