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Formula: Na2BaAl4Si4O16
Tectosilicate (framework silicate), feldspar group, forms a series with
stronalsite
Specific gravity: 3.05 calculated
Hardness: 6
Streak: White
Colour: White
Solubility: Decomposed by hydrochloric acid
Common impurities: Mn,Mg,Ca,K
Environments
Metamorphic environments
Hydrothermal environments
Banalsite is a rare mineral which was the first barium aluminium silicate to be described with sodium as the dominant alkali;
it forms under hydrothermal or metamorphic conditions
(MW).
Localities
At the type locality, the Benallt Mine, Rhiw, Aberdaron, Gwynedd, Wales, UK, banalsite is found in veins and vugs where it is
associated with a suite of minerals believed to have been derived from hydrothermal activity involving manganese-rich fluids exhaled
onto the Ordovician sea floor. The banalsite typically forms thin bands of coarsely crystalline material cutting dark spotted
manganese ore, and crystals of banalsite to 2 mm have been found in small cavities in the ore body. In all occurrences in the
mine banalsite is associated with calcite, baryte,
tephroite, alleghanyite,
jacobsite, biotite,
natrolite and harmotome
(AM 30.85, MW, Mindat, HOM).
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