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McCall, G. J. H. (1965) A meteorite of unique type from Western Australia: The Mount Egerton stony-iron. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (270) 241-249 doi:10.1180/minmag.1965.035.270.01

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Reference TypeJournal (article/letter/editorial)
TitleA meteorite of unique type from Western Australia: The Mount Egerton stony-iron
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsMcCall, G. J. H.Author
Year1965 (June)Volume35
Issue270
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_35/35-270-241.pdf+
DOIdoi:10.1180/minmag.1965.035.270.01Search in ResearchGate
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Mindat Ref. ID5870Long-form Identifiermindat:1:5:5870:8
GUID0
Full ReferenceMcCall, G. J. H. (1965) A meteorite of unique type from Western Australia: The Mount Egerton stony-iron. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (270) 241-249 doi:10.1180/minmag.1965.035.270.01
Plain TextMcCall, G. J. H. (1965) A meteorite of unique type from Western Australia: The Mount Egerton stony-iron. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (270) 241-249 doi:10.1180/minmag.1965.035.270.01
In(1965) Mineralogical Magazine Vol. 35 (270) Mineralogical Society
Abstract/NotesSummaryA unique meteorite, the existence of which has been known since 1941 but which had been lost, has now been relocated in the form of fragments in two separate collections. Though material available is limited to small fragments, it is sufficient to reveal the principal characteristics of the parent mass, which was a variable body composed of stony material not dissimilar from that of the unbrecciated enstatite-achondrite of Shallowater, Texas, U.S.A., and nickel-iron not dissimilar from the ‘pseudo-octahedrite’ of Horse Creek, Colorado, U.S.A. There is evidence suggesting that it was a stony-iron of a hitherto unrecorded type, and that silicate material predominated.


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