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Axon, H. J., Smith, P. L. (1970) A metallographic and microprobe study of the metal phases in the Weekeroo Station meteorite. Mineralogical Magazine, 37 (290) 670-673 doi:10.1180/minmag.1970.037.290.04

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Reference TypeJournal (article/letter/editorial)
TitleA metallographic and microprobe study of the metal phases in the Weekeroo Station meteorite
JournalMineralogical Magazine
AuthorsAxon, H. J.Author
Smith, P. L.Author
Year1970 (June)Volume37
Issue290
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_37/37-290-670.pdf+
DOIdoi:10.1180/minmag.1970.037.290.04Search in ResearchGate
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Mindat Ref. ID6364Long-form Identifiermindat:1:5:6364:1
GUID0
Full ReferenceAxon, H. J., Smith, P. L. (1970) A metallographic and microprobe study of the metal phases in the Weekeroo Station meteorite. Mineralogical Magazine, 37 (290) 670-673 doi:10.1180/minmag.1970.037.290.04
Plain TextAxon, H. J., Smith, P. L. (1970) A metallographic and microprobe study of the metal phases in the Weekeroo Station meteorite. Mineralogical Magazine, 37 (290) 670-673 doi:10.1180/minmag.1970.037.290.04
In(1970, June) Mineralogical Magazine Vol. 37 (290) Mineralogical Society
Abstract/NotesSummaryThe kamacite contains a general precipitation of micrometre-sized particles of exsolved taenite. Larger particles are found decorating Neumann lines and at kamacite grain boundaries. The coexisting kamacite and taenite appear to have nickel contents of 6·4 % and about 53%, which are consistent with a temperature of about 330–60 °C on the binary iron-nickel equilibrium diagram.


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