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Hexamolybdenum information


Hexamolybdenum
General
CategoryNative mineral alloy
Formula
(repeating unit)
(Mo,Ru,Fe,Ir,Os)
IMA symbolHmo[1]
Strunz classification1.XX.00
Crystal systemHexagonal
Crystal classDihexagonal dipyramidal (6/mmm)
H-M symbol: (6/m 2/m 2/m)
Space groupP63/mmc
Unit cella = 2.7506, c = 4.4318 [Å]
V = 29.04 Å3, Z = 2
Identification
Crystal habitInclusions and microscopic crystals
Specific gravity11.90 (calculated)
References[2][3][4]

Hexamolybdenum is a molybdenum dominant alloy discovered during a nanomineralogy investigation of the Allende meteorite.[4] Hexamolybdenum was discovered in a small ultrarefractory inclusion within the Allende meteorite.[4] This inclusion has been named ACM-1.[4] Hexamolybdenum is hexagonal, with a calculated density of 11.90 g/cm3.[4] The new mineral was found along with allendeite.[4] These minerals, are believed to demonstrate conditions during the early stages of the Solar System, as is the case with many CV3 carbonaceous chondrites such as the Allende meteorite.[4] Hexamolybdenum lies on a continuum of high-temperature alloys that are found in meteorites and allows a link between osmium, ruthenium, and iron rich meteoritic alloys.[4] The name hexamolybdenum refers to the crystal symmetry (primitive hexagonal) and the molybdenum rich composition.[4] The Allende meteorite fell in 1969 near Pueblito de Allende, Chihuahua, Mexico.[4]

  1. ^ 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.
  2. ^ Mindat.org
  3. ^ Webmineral data
  4. ^ a b c d e f g h i j Beckett, John R.; Rossman, George R. (2014). "Allendeite (Sc3Zr4O12 and hexamolybdenum (Mo, Ru, Fe), two new minerals from an ultrarefractory inclusion from the Allende meteorite". American Mineralogist. 99 (4): 654–666. Bibcode:2014AmMin..99..654M. doi:10.2138/am.2014.4667. S2CID 94914236.

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