Dagenaisite

dagenaisite

dugganite

eurekadumpite

cinnabar

Images

Formula: Zn3Te6+O6
Tellurate
Crystal System: Monoclinic
Specific gravity: 6.0 calculated
Hardness: Less than 2
Streak: White
Colour: Green, light greenish grey
Solubility: At room temperature, slowly soluble in dilute hydrochloric acid and rapidly soluble in concentrated hydrochloric acid
Environments

Hydrothermal environments

Dagenaisite is a relatively new mineral, approved in 2017.

Localities

The type locality, the Gold Chain Mine, Mammoth, Tintic Mining District, Juab County, Utah, USA, exploited a polymetallic gold - silver - copper - lead - zinc vein deposit emplaced in dolostone. The upper portion of the deposit is almost completely oxidised.
Dagenaisite was collected underground; it is associated with cinnabar, dugganite, eurekadumpite and gold in vugs in a matrix composed of quartz and dolomite. Altered remnants, probably of hessite, are embedded in the matrix. Other minerals identified in the general assemblage include adamite, arseniosiderite, atelestite, baryte, beudantite, conichalcite, hemimorphite, kettnerite, malachite, mimetite, mixite, olivenite and rosasite.
Dagenaisite is clearly a late stage secondary phase formed by the oxidative alteration of earlier tellurium- and zinc- bearing minerals, probably hessite and sphalerite (CM 55.867-873).

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