| Taenite | |
|---|---|
 Widmanstätten patterns of kamacite and taenite, from a meteorite currently in the Natural History Museum, London. | |
| General | |
| Category | Metals and intermetallic alloys |
| Formula (repeating unit) | γ-(Ni,Fe) |
| IMA symbol | Tae[1] |
| Strunz classification | 1.AE.10 |
| Crystal system | Isometric |
| Crystal class | Hexoctahedral (m3m) H-M symbol: (4/m 3 2/m) |
| Space group | Fm3m |
| Identification | |
| Color | metallic grayish to white |
| Cleavage | None |
| Fracture | Hackly fracture |
| Tenacity | Malleable, flexible |
| Mohs scale hardness | 5–5.5 |
| Luster | metallic |
| Streak | light gray |
| Diaphaneity | Opaque |
| Specific gravity | 7.8–8.22 |
| Other characteristics | magnetic, not radioactive |
| References | [2][3] |
Taenite is a mineral found naturally on Earth mostly in iron meteorites. It is an alloy of iron and nickel, with a chemical formula of Fe,Ni and nickel proportions of 20% up to 65%.
The name is derived from the Greek ταινία for "band, ribbon". Taenite is a major constituent of iron meteorites. In octahedrites it is found in bands interleaving with kamacite forming Widmanstätten patterns, whereas in ataxites it is the dominant constituent. In octahedrites a fine intermixture with kamacite can occur, which is called plessite.
Taenite is one of four known Fe-Ni meteorite minerals: The others are kamacite, tetrataenite, and antitaenite.
- ^ 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.
- ^ Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W.; Nichols, Monte C. (2005). "Taenite" (PDF). Handbook of Mineralogy. Mineral Data Publishing. Retrieved 14 March 2022.
- ^ http://webmineral.com/data/Taenite.shtml Archived 2021-01-22 at the Wayback Machine Webmineral data