Gabrielite | |
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General | |
Category | Sulfide mineral |
Formula (repeating unit) | Tl6Ag3Cu6(As,Sb)9S21 |
IMA symbol | Gab[1] |
Strunz classification | 2.HD.60 |
Crystal system | Triclinic |
Crystal class | Pinacoidal (1) (same H-M symbol) |
Space group | P1 |
Unit cell | a = 12.138, b = 12.196 c = 15.944 [Å]; α = 78.537° β = 84.715°, γ = 60.47°; Z = 6 |
Identification | |
Color | Grey to black |
Crystal habit | Pseudo Hexagonal |
Twinning | Common, with (100) as twin plane |
Cleavage | Perfect on {001} |
Fracture | uneven |
Mohs scale hardness | 1.5 - 2 |
Luster | Metallic |
Streak | Blackish red |
Diaphaneity | Opaque |
Density | 5.38 g/cm3 |
Birefringence | weak 470nm R=30.53% 546nm R=29.1% 589nm R=27.94% 650nm R=26.35% |
References | [2][3] |
Gabrielite is an extremely rare thallium sulfosalt mineral with a chemical formula of Tl6Ag3Cu6(As,Sb)9S21[2] or Tl2AgCu2As3S7.[3]
It was first reported in 2002 for its occurrence in the Lengenbach quarry, Binntal, Valais, Switzerland. According to Faszination Lengenbach (2008), only 2 specimens are known. A few dozen tiny fragments like the one pictured are circulating few collections. Named after Walter Gabriel (born 1943), a Swiss mineral photographer.[2][3] This region was transformed during the greenschist-garnet/amphibolite facies of metamorphism. Due to this many rare sulfosalts like gabrielite are found in this part of Switzerland.