Brockite | |
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General | |
Category | Phosphate mineral |
Formula (repeating unit) | (Ca,Th,Ce)PO4·H2O |
IMA symbol | Bck[1] |
Strunz classification | 8.CJ.45 |
Crystal system | Hexagonal |
Crystal class | Trapezohedral (622) H-M symbol: (622) |
Space group | P6222 or P6422 |
Unit cell | a = 6.98 Å, c = 6.40 Å; Z = 3 |
Identification | |
Color | Reddish brown, yellow (red brown due to inclusions of hematite) |
Crystal habit | Rarely as Stubby hexagonal prisms rare; common as granular massive aggregates, cryptocrystalline |
Cleavage | None observed |
Fracture | Conchoidal |
Tenacity | Brittle |
Mohs scale hardness | 3 - 4 |
Luster | Greasy to vitreous |
Diaphaneity | Translucent to opaque |
Specific gravity | 3.9 (measured) |
Optical properties | Uniaxial (+) |
Refractive index | nω = 1.680 nε = 1.695 |
Birefringence | δ = 0.015 |
Other characteristics | Radioactive |
References | [2][3][4] |
Brockite is a rare earth phosphate mineral with formula: (Ca,Th,Ce)PO4·H2O. It crystallizes in the hexagonal system in the chiral space group 180 or its enantiomorph 181. It is typically granular to massive with only rare occurrence of stubby crystals. It is radioactive due to the thorium content.