Markcooperite

markcooperite

chlorargyrite

iodargyrite

khinite

Images

Formula: Pb2(UO2)TeO6
Tellurate, uranyl mineral, lead-bearing mineral
Crystal System: Monoclinic
Specific gravity: 8.496 calculated for the empirical formula
Hardness: 3
Streak: Light orange
Colour: Orange
Luminescence: Not fluorescent under UV
Solubility: In dilute hydrochloric acid, markcooperite immediately decomposes, turning white and opaque, and then dissolves slowly
Environments

Hydrothermal environments

Localities

At the type locality, the Aga Mine, Otto Mountain, Baker, Soda Mountains, Silver Lake Mining District, San Bernardino County, California, USA, markcooperite is very rare and occurs on fracture surfaces and in small vugs in quartz veins. Species observed in direct association with markcooperite include bromine-rich chlorargyrite, iodargyrite, khinite-4O, wulfenite and four tellurates, housleyite, ottoite, thorneite and timroseite. Other species identified in the assemblages include acanthite, anglesite, atacamite, boleite, brochantite, burckhardtite, calcite, caledonite, celestine, cerussite, chalcopyrite, chrysocolla, devilline, diaboleite, eztlite, fluorite, fornacite, galena, goethite, gold, hessite, jarosite, kuranakhite, linarite, malachite, mimetite, mottramite, munakataite, murdochite, muscovite, perite, phosphohedyphane, plumbojarosite, pyrite, schieffelinite, vanadinite, vauquelinite, and two other new minerals, paratimroseite and telluroperite.
Markcooperite and most of the other secondary minerals of the quartz veins are interpreted as having formed from the partial oxidation of primary sulphides, such as galena, and tellurides, such as hessite, during or following brecciation of the quartz veins. The uranium may have originated from one or more primary uranium-bearing phases (possibly uraninite in the form of inclusions).
Markcooperite crystals are pseudotetragonal prisms ranging from tiny, thin, tapering prisms, less than 5 µm in length to larger squat prisms to 0.2 mm in length. Most commonly, the mineral occurs as botryoidal aggregates to 0.3 mm across, which consist of tightly intergrown crystals. Markcooperite is orange and transparent, with a light orange streak and adamantine lustre (AM 95.10.1554-1559).
Markcooperite from the Aga Mine - Image

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