Tugarinovite

tugarinovite

uraninite

molybdenite

zircon

Images

Formula: MoO2
Valence: Mo4+O2
Simple oxide of molybdenum Mo4+
Crystal system: Monoclinic
Specific gravity: 6.58 calculated
Hardness: 4½
Streak: Greenish grey
Colour: Dark lilac-brown
Solubility: Insoluble in hot hydrochloric or sulphuric acid, but is dissolved very slowly by boiling concentrated nitric acid
Electrical: Conductor of electricity
Environments

Volcanic igneous environments
Hydrothermal environments

Localities

At the type locality, the Lenskoye Mo-U deposit, Amur Oblast, Russia, tugarinovite occurs as prismatic or thick tabular crystals 0.5 to 1.5 mm in size with a greasy to metallic lustre. It occurs in quartz metasomatites associated with uraninite, molybdenite, zircon and galena.
Tugarinovite is considered to be of hypogene origin, formed in a reducing medium with deficiency of sulphur (AM 66.438-439).
Partial to complete pseudomorphism by wulfenite occurs in oxidised material (AM 73.189-199).

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