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Mackinawite
Iron nickel sulfide mineral
Iron nickel sulfide mineral
| Field | Value |
|---|---|
| name | Mackinawite |
| category | Sulfide mineral |
| image | Mackinawite-95018.jpg |
| imagesize | 260px |
| formula | (where x=0 to 0.11) |
| IMAsymbol | Mkw |
| molweight | 85.42 g/mol |
| strunz | 2.CC.25 |
| system | Tetragonal |
| class | Ditetragonal dipyramidal (4/mmm) |
| H-M symbol: (4/m 2/m 2/m) | |
| symmetry | P4/nmm |
| unit cell | a = 3.67 Å, c = 5.03 Å; Z = 2 |
| color | Bronze to white grey |
| habit | As well-formed thin tabular crystals; massive, fine-feathery |
| cleavage | Perfect on {001} |
| mohs | 2.5 |
| luster | Metallic |
| streak | Black |
| gravity | 4.17 |
| diaphaneity | Opaque |
| references |
H-M symbol: (4/m 2/m 2/m) Mackinawite ( ) is an iron sulfide mineral, which can contain nickel substituting for iron(II), with as chemical formula (where x = 0 to 0.11). As indicated by its chemical composition, Fe(1+×), Fe is present with an excess of × over S, and it is thus an iron-rich, or a sulfur-deficient, iron monosulfide mineral. The mineral crystallizes in the tetragonal crystal system and has been described as a distorted, close packed, cubic array of S atoms with some of the gaps filled with Fe. Mackinawite 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. It was first described in 1962 for an occurrence in the Mackinaw mine, Snohomish County, Washington for which it was named.
Occurrence
Mackinawite occurs in serpentinized peridotites as a hydrothermal alteration product, in meteorites, and in association with chalcopyrite, cubanite, pentlandite, pyrrhotite, greigite, maucherite, and troilite. Mackinawite also occurs in reducing environments such as freshwater and marine sediments as a result of the metabolism of iron and sulfate-reducing bacteria.
In anoxic environments, mackinawite is formed by the reaction of HS− with either Fe2+ ions or with Fe metal.{{cite journal
Transformations in the environment
Depending on the redox conditions mackinawite can form more stable phases such as greigite and ultimately pyrite,{{cite book | editor-last1 = Amend | editor-first1 = J.P. | editor-last2 = Edwards | editor-first2 = K.J. | editor-last3 = Lyons | editor-first3 = T.W. | doi-access = free
References
References
- Warr, L.N.. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine.
- [https://www.mineralienatlas.de/lexikon/index.php/MineralData?mineral=Mackinawite Mineralienatlas]
- [http://rruff.geo.arizona.edu/doclib/hom/mackinawite.pdf Handbook of Mineralogy]
- [http://webmineral.com/data/Mackinawite.shtml Webmineral data]
- [http://www.mindat.org/min-2512.html Mindat]
- {{cite OED2. mackinawite
- (1970). "Structural refinement and composition of mackinawite". Carnegie Institute of Washington Geophysical Laboratory Annual Report.
- Csákberényi-Malasics, D., Rodriguez-Blanco, J.D., Kovács Kis, V., Rečnik, A., Benning, L.G., and Pósfai, M. (2012) Structural properties and transformations of precipitated FeS. Chemical Geology, 294–295, 249–258. doi: 10.1016/j.chemgeo.2011.12.009.
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