Abramovite
Abramovite 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 1 mm × 0.2 mm in size, and is characterized by its non-commensurate structure.[5]
| Abramovite | |
|---|---|
 | |
| General | |
| Category | Sulfides and Sulfosalts |
| Formula (repeating unit) | Pb2SnInBiS7 |
| IMA symbol | Abm[1] |
| Strunz classification | 2.HF.25a (10th edition) |
| Dana classification | 03.01.03.03 |
| Crystal system | Triclinic |
| Crystal class | Pinacoidal (1) (same H-M symbol) |
| Space group | P1 |
| Unit cell | a = 23.4 Å, b = 5.77 Å c = 5.83 Å; α = 89.1° β = 89.9°, γ = 91.5°; Z = 4 |
| Identification | |
| Formula mass | 1,066.44 g/mol |
| Color | Silver gray |
| Crystal habit | Encrustations - Forms crust-like aggregates on matrix |
| Twinning | Lamellar on {100} |
| Cleavage | Perfect on {100} |
| Luster | Metallic |
| Streak | Black |
| Diaphaneity | Opaque |
| References | [2][3][4][5] |
Etymology and history
Abramovite is named after the mineralogist Dmitry Vadimovich Abramov (born 1963) of the A.E. Fersman Museum, Russia.[2]
It was discovered as fumarole crust on the Kudriavy (Kudryavyi) volcano, Iturup Island, Kuril Islands, Sakhalin Oblast, Far East Region, Russia.[5]
Formation
Abramovite is a product of precipitation from fumarolic gases (600 °C [1,112 °F]) in an active stratovolcano.[2]
See also
References
- Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- "Handbook of Mineralogy" (PDF). Archived from the original (PDF) on 2019-05-08. Retrieved 2011-04-28.
- Mindat.org
- Webmineral.com Webmineral Data
- Yudovskaya, M.A.; Trubkin, N.V.; Koporulina, E.V.; Belakovsky, D.I.; Mokhov, A.V.; Kuznetsova, M.V.; Golovanova, T.I. (2007). "Abramovite, Pb2SnInBiS7, a new mineral species from fumaroles of the Kudryavy Volcano, Kurile Islands". Zapiski Rossiiskogo Mineralogicheskogo Obshchestva (in Russian): 37–43. Bibcode:2008GeoOD..50..551Y. doi:10.1134/S1075701508070052. ISSN 0869-6055. S2CID 140650406.
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