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A review of hexaferrum based on new mineralogical data
Luleå University of Technology. (Department of Civil Engineering and Natural Resources)ORCID iD: 0000-0002-1298-0320
(English)In: Mineralogical magazine, ISSN 0026-461X, E-ISSN 1471-8022Article in journal (Refereed) Epub ahead of print
Abstract [en]

Hexaferrum, defined as an hcp Fe mineral containing varying amounts of Ru, Os, or Ir(Mochalov et al. 1998) was re-examined in the light of new analyses of similar alloys from the Loma Peguera and Loma Larga chromitites, in the central part of Loma Caribe peridotite, Cordillera Central of the Dominican Republic, together with a review of the phase chemistry inthe Fe-Ni-Ir and Fe-Ru-Ir systems. We conclude that the hcp (Fe,Ir) mineral corresponds to theε-phase of Raub et al. (1964) and should be differentiated from hexaferrum [(Fe,Os) and(Fe,Ru)] because it is separated by one to two miscibility gaps and therefore is not a continuous solid solution with Fe.

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URN: urn:nbn:se:ltu:diva-68360DOI: 10.1180/mgm.2018.86OAI: oai:DiVA.org:ltu-68360DiVA, id: diva2:1197845
Available from: 2018-04-15 Created: 2018-04-15 Last updated: 2018-04-15

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Publisher's full texthttps://www.cambridge.org/core/journals/mineralogical-magazine/article/review-of-hexaferrum-based-on-new-mineralogical-data/F6AA04FCE5163D52C9774D6D1CAD5D15

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