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A review of hexaferrum based on new mineralogical data
Cabri Consulting Inc, Ottawa, Canada.
Luleå University of Technology, Department of Civil, Environmental and Natural Resources Engineering, Geosciences and Environmental Engineering.ORCID iD: 0000-0002-1298-0320
2018 (English)In: Mineralogical magazine, ISSN 0026-461X, E-ISSN 1471-8022, Vol. 82, no 3, p. 531-538Article in journal (Refereed) Published
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.

Place, publisher, year, edition, pages
Mineralogical Society of Great Britain and Ireland , 2018. Vol. 82, no 3, p. 531-538
Keywords [en]
hexaferrum, nomenclature, Fe – Ni – Ir, Fe – Ru – Ir, ternary systems
National Category
Geology Geochemistry
Research subject
Applied Geochemistry
Identifiers
URN: urn:nbn:se:ltu:diva-68360DOI: 10.1180/mgm.2018.86ISI: 000452140100006Scopus ID: 2-s2.0-85048723922OAI: oai:DiVA.org:ltu-68360DiVA, id: diva2:1197845
Note

Validerad;2018;Nivå 1;2018-12-04 (marisr);Bibliografisk uppgift: This paper is published as part of a thematic set in memory of Professor Hazel M. Prichard

Available from: 2018-04-15 Created: 2018-04-15 Last updated: 2019-02-27Bibliographically approved

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