Paradocrasite

paradocrasite

lollingite

stibarsen

antimony

Images

Formula: Sb2(Sb,As)2
A very rare, natural antimony-rich, arsenic-bearing alloy
Crystal System: Monoclinic
Specific gravity: 6.5 measured, 6.44 calculated
Hardness: 3
Streak: Black
Colour: Silver-white
Environments

Metamorphic environments

Localities

The type locality is Broken Hill, Broken Hill district, Yancowinna county, New South Wales, Australia. In a museum hand specimen purportedly from this locality, paradocrasite is mainly an aggregate of small, diversely oriented, brilliant silver-white, stubby prisms, each about 0.5 mm long, embedded in a matrix of white calcite. Some prisms are striated parallel to the long axis. A few prisms are curved. The ends of the prisms are rough, showing intersecting domains that represent complex, repeated twins. A few nests of curved, grooved pseudohexagonal plates are also present. Paradocrasite is brittle, crushing readily to fine dust.
Some doubt has been expressed as to whether this specimen really originated from Broken Hill (AM 56.1127-1146).
The paradocrasite replaces calcite, and is associated with antimony-bearing löllingite, stibarsen and calcite (HOM).

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