Tugarinovite | |
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General | |
Category | Oxide mineral |
Formula (repeating unit) | MoO2 |
IMA symbol | Tug[1] |
Strunz classification | 4.DB.05 |
Crystal system | Monoclinic |
Crystal class | Prismatic H-M symbol (2/m) |
Space group | P21/c (no. 14) |
Unit cell | a = 5.6 Å, b = 4.85 Å, c = 5.53 Å; β = 119.37° |
Identification | |
Color | Dark lilac-brown |
Crystal habit | Crystals are tabular striated prisms |
Twinning | Polysynthetic |
Mohs scale hardness | 4.6 |
Luster | Greasy to metallic |
Streak | Greenish gray |
Diaphaneity | Semitransparent |
Specific gravity | 6.58 (calculated) |
Optical properties | Biaxial |
Pleochroism | Light gray to dark pink; pale yellow to bluish olive-brown in reflected light |
References | [2][3][4] |
Tugarinovite is a rare molybdenum oxide mineral with formula MoO2. It occurs as a primary mineral phase associated with metasomatism in a sulfur deficient reducing environment. In the type locality it occurs with uraninite, molybdenite, galena, zircon and wulfenite.[2]
Tugarinovite was first described for an occurrence in the Lenskoye molybdenum–uranium deposit in the Amurskaya Oblast, Far-Eastern Region, Russia. It was named for geochemist Ivan Alekseevich Tugarinov of the Vernadskii Institute in Moscow.[2][3] In addition to its type locality in Russia it has been reported from the Allende meteorite in Chihuahua, Mexico, the Nansei Archipelago of Japan and Bohemia in the Czech Republic.[3]