| 词条 | Haxonite |
| 释义 |
| name = Haxonite | image = | alt = | caption = | category = Native element minerals | formula = (Fe,Ni)23C6 | molweight = | strunz = 1.BA.10 | system = Isometric Unknown space group | symmetry = | unit cell = | color = | colour = | habit = | twinning = | cleavage = | fracture = | tenacity = | mohs = {{frac|5|1|2}} - 6 | luster = | streak = | diaphaneity = | gravity = | density = | polish = | opticalprop = | refractive = | birefringence = | pleochroism = | 2V = | dispersion = | extinction = | length fast/slow = | fluorescence = | absorption = | melt = | fusibility = | diagnostic = | solubility = | impurities = | alteration = | other = | prop1 = | prop1text = | references = }}Haxonite is an iron nickel carbide mineral found in iron meteorites and carbonaceous chondrites. It has a chemical formula of (Fe,Ni)23C6, crystallises in the cubic crystal system and has a Mohs hardness of {{frac|5|1|2}} - 6.[1][2] It was first described in 1971, and named after Howard J. Axon (1924–1992), metallurgist at the University of Manchester, Manchester, England. Co-type localities are the Toluca meteorite, Xiquipilco, Mexico and the Canyon Diablo meteorite, Meteor Crater, Coconino County, Arizona, US.[1] It occurs associated with kamacite, taenite, schreibersite, cohenite, pentlandite and magnetite.[2] See also
References1. ^1 Mindat.org {{Meteorites}}2. ^1 Handbook of Mineralogy 6 : Carbide minerals|Iron minerals|Nickel minerals|Meteorite minerals|Cubic minerals|Native element minerals |
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