Trippkeite

trippkeite

cuprite

malachite

olivenite

Images

Formula: Cu2+As3+2O4
Arsenite, minium group
Crystal System: Tetragonal
Specific gravity: 4.8 measured, 4.49 calculated
Hardness: 4
Streak: Pale blue
Colour: Brilliant greenish-blue, pistachio-green; pale bluish green in transmitted light; with neon-blue internal reflections
Solubility: Readily soluble in hydrochloric or nitric acid
Environments

Plutonic igneous environments
Hydrothermal environments

Localities

At the type locality, Copiapó Province, Atacama, Chile, trippkeite occurs in a copper deposit associated with cuprite, malachite, olivenite and chalcopyrite (HOM).
Trippkeite from Copiapó Province - Image

At the Bou Azzer mining district, Drâa-Tafilalet Region, Morocco, malachite is associated with trippkeite as a later-generation cover on the trippkeite. The cobalt - nickel - arsenic mineralisation is associated with serpentinite, dolostone, granite, gabbro and quartz diorite along various secondary structures such as faults and brecciated zones, and is distinctly different from that at the Albert Silver mine (see below) (R&M 89.5.416-423).

At the Albert silver mine, Thembisile Hani Local Municipality, Nkangala District Municipality, Mpumalanga, South Africa, the ore deposit occurs in a fissure zone of vertical quartz veins in porphyritic granite. The mineral assemblage comprises copper, silver, lead, antimony and uranium. Copper and silver are the most abundant. Uranium occurs as microcrystals of uraninite, together with quartz, magnetite, hematite and purple fluorite. The principal sulphides in order of abundance are bornite, pyrite, chalcopyrite, tetrahedrite and chalcocite. In addition, subordinate quantities of arsenopyrite, sphalerite, galena and jamesonite occur. Hematite is a secondary product of pyrite. The sulphide paragenetic sequence is pyrite and arsenopyrite, sphalerite and tetrahedrite, galena and jamesonite, bornite and chalcocite, and, lastly, chalcopyrite.
Trippkeite occurs in association with malachite; the minerals are a mixture of each other and responsible for the pale green coating in and on quartz crystals (R&M 89.5.416-423)
Trippkeite from the Albert Silver Mine - Image

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