Curite
Curite | |
---|---|
Curite | |
General | |
Category | Oxide mineral |
Formula (repeating unit) | Pb3(UO2)8O8(OH)6·3(H2O) |
Strunz classification | 04.GB.55 |
Crystal system | Orthorhombic |
Identification | |
Color | Yellow, reddish orange, brownish yellow. |
Crystal habit | Massive, acicular, compact earthy. |
Crystal symmetry | Orthorhombic (2/m 2/m 2/m) dipyramidal |
Cleavage | {100}, imperfect |
Tenacity | Brittle |
Mohs scale hardness | 4-5 |
Luster | Adamantine |
Streak | Orange |
Diaphaneity | Transparent |
Specific gravity | 6.98 - 7.4 |
Optical properties | Biaxial (-) |
Refractive index | nα = 2.060 nβ = 2.110 nγ = 2.150 |
Birefringence | .090 |
Pleochroism | Visible: X = b = pale yellow, Y = a = light red-orange, Z = c = dark red-orange |
2V angle | 70° |
Ultraviolet fluorescence | Yes |
Other characteristics | Radioactive |
References | [1][2] |
Curite is a lead uranium oxide mineral with formula: Pb3(UO2)8O8(OH)6·3(H2O). It is named after the physicists Marie and Pierre Curie, who are both known for their work on radioactivity. The type locality is the Shinkolobwe Mine.[1]
References
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