Bellbergite

bellbergite

pyrrhotite

thomsonite-(Ca)

ettringite

Images

Formula: (K,Ba,Sr)2Sr2Ca2(Ca,Na)4(Si,Al)36O72.30H2O
Tectosilicate (framework silicate), zeolite group, barium- and strontium- bearing mineral
Crystal System: Hexagonal
Specific gravity: 2.2 measured 2.19 calculated
Hardness: 5
Streak: White
Colour: Colourless to white
Environments

Volcanic igneous environments

Localities

The Cerro Sapo dyke, Ayopaya Province, Cochabamba, Bolivia, consists of rhythmically-layered ankerite and baryte with bands or irregular patches of monomineralic dark blue sodalite with crystals reaching up to 9 cm. The dyke cross-cuts nepheline syenite, the contact between which is strongly brecciated with an intense sodaliteankerite stockwork and narrow zones of fenitisation. The dyke contains a diverse suite of minor minerals including calcite, microcline, natrolite, analcime, sulphides (galena, sphalerite, pyrite and chalcopyrite) as well as rare-earth-element – strontiumthorium -rich minerals including strontianite, strontium-bearing apatite, goyazite, mckelveyite and bellbergite (MM 86.282-306).

At the type locality, the Bellerberg volcano, Vordereifel, Mayen-Koblenz District, Rhineland-Palatinate, Germany, bellbergite occurs at the contacts of calcium-rich xenoliths in leucite tephrite. Cavities in the hybrid zone are lined with crystals of sanidine, clinopyroxene and altered pyrrhotite, on which bellbergite and spheres of thomsonite-(Ca) were deposited and succeeded by tufts of ettringite (AM 79.570). Other associates of bellbergite include willhendersonite, gismondine, jasmundite, mayenite, chlormayenite, srebrodolskite, calcio-olivine and portlandite (HOM, Mindat).

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