Coffinite | |
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General | |
Category | Nesosilicate |
Formula (repeating unit) | U(SiO4)1−x(OH)4x |
IMA symbol | Cof[1] |
Strunz classification | 9.AD.30 |
Crystal system | Tetragonal |
Crystal class | Ditetragonal dipyramidal (4/mmm) H-M symbol: (4/m 2/m 2/m) |
Space group | I41/amd |
Unit cell | a = 6.97 Å, c = 6.25 Å; Z = 4 |
Identification | |
Color | Black (from organic inclusions; pale to dark brown in thin section |
Crystal habit | Rarely as crystals, commonly as colloform to botryoidal incrustations, fibrous, pulverulent masses |
Fracture | Irregular to subconchoidal |
Tenacity | Brittle to friable |
Mohs scale hardness | 5–6 |
Luster | Dull to adamantine |
Streak | Grayish black |
Diaphaneity | Opaque, transparent on thin edges |
Specific gravity | 5.1 |
Optical properties | Uniaxial (+/−) |
Refractive index | nα = 1.730–1.750 nβ = 1.730–1.750 |
Birefringence | δ = 1.730 |
Pleochroism | Moderate; pale yellow-brown parallel to and medium brown perpendicular to long axis |
Alters to | Metamict |
Other characteristics | Radioactive 72.63% (U) |
References | [2][3][4][5][6][7][8][9][10][11][12][13][14] |
Coffinite is a uranium-bearing silicate mineral with formula: U(SiO4)1−x(OH)4x.
It occurs as black incrustations, dark to pale-brown in thin section. It has a grayish-black streak. It has a brittle to conchoidal fracture. The hardness of coffinite is between 5 and 6.
It was first described in 1954 for an occurrence at the La Sal No. 2 Mine, Beaver Mesa, Mesa County, Colorado, US,[5] and named for American geologist Reuben Clare Coffin (1886–1972).[3] It has widespread global occurrence in Colorado Plateau-type uranium ore deposits of uranium and vanadium. It replaces organic matter in sandstone and in hydrothermal vein type deposits.[3] It occurs in association with uraninite, thorite, pyrite, marcasite, roscoelite, clay minerals and amorphous organic matter.[3]