Abramovite | |
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General | |
Category | Sulfides and Sulfosalts |
Chemical formula | Pb2SnInBiS7 |
Strunz classification | 02.HF.25a (8th edition) |
Dana classification | 03.01.03.03 |
Unit cell | a = 23.4 Å, b = 5.77 Å, c = 5.83 Å; α = 89.1°, β = 89.9°, γ = 91.5° |
Identification | |
Molar mass | 1,066.44 g/mol |
Color | Silver gray |
Crystal habit | Encrustations - Forms crust-like aggregates on matrix |
Crystal system | Triclinic - Pinacoidal; Space group = P1 |
Twinning | Lamellar on {100} |
Cleavage | Perfect on {100} |
Luster | Metallic |
Streak | Black |
Diaphaneity | Opaque |
References | [1][2][3][4] |
Abramotive is a very rare mineral from the sulfides and sulfosalt categories. It has the chemical formula Pb2SnInBiS7. It occurs as tiny elongated lamellar-shaped crystals, up 1mm × 0.2mm in size, and is characterized by its non-commensurate structure.[4]
Abramovite is named after the mineralogist Dmitry Vadimovich Abramov (1963–) of the A.E. Fersman Museum, Russia.[1]
It was discovered as fumarole crust on the Kudriavy volcano|Kudriavy (Kudryavyi) volcano, Iturup Island, Kuril Islands, Sakhalin Oblast, Far East Region, Russia.[4]
Abramovite is a product of precipitation from fumarolic gases (600°C) in an active stratovolcano.[1]