Mackinawite
Mackinawite | |
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Mackinawite | |
General | |
Category | Sulfide mineral |
Formula (repeating unit) | (Fe,Ni)1 + xS (where x = 0 to 0.11) |
Strunz classification | 02.CC.25 |
Crystal symmetry | Tetragonal 4/m 2/m 2/m |
Unit cell | a = 3.67 Å, c = 5.03 Å; Z=2 |
Identification | |
Formula mass | 85.42 g |
Color | Bronze to white grey |
Crystal habit | As well-formed thin tabular crystals; massive, fine-feathery |
Crystal system | Tetragonal - ditetragonal dipyramidal |
Cleavage | Perfect on {001} |
Mohs scale hardness | 2.5 |
Luster | Metallic |
Streak | Black |
Diaphaneity | Opaque |
Specific gravity | 4.17 |
References | [1][2][3] |
Mackinawite is an iron nickel sulfide mineral with formula (Fe,Ni)1 + xS (where x = 0 to 0.11). It crystallizes in the tetragonal crystal system and occurs as opaque bronze to grey-white tabular crystals and anhedral masses. It has a Mohs hardness of 2.5 and a specific gravity of 4.17.
Occurrence
It occurs in serpentinized peridotites as a hydrothermal alteration product. It also is found in the reducing environment of fine grained river sediments, possibly produced by the action of magnetotactic and sulfate-reducing bacteria. It has also been reported from meteorite occurrences. It occurs in association with chalcopyrite, cubanite, pentlandite, pyrrhotite, greigite, maucherite and troilite.[1]
It was first described in 1962 for an occurrence in the Mackinaw mine, Snohomish County, Washington for which it was named.[3]
See also
References
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