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Graham, A. L., Easton, A. J., Hutchison, R. (1977) The Mayo Belwa meteorite: a new enstatite achondrite fall. Mineralogical Magazine, 41 (320) 487-492 doi:10.1180/minmag.1977.041.320.10

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Reference TypeJournal (article/letter/editorial)
TitleThe Mayo Belwa meteorite: a new enstatite achondrite fall
JournalMineralogical MagazineISSN0026-461X
AuthorsGraham, A. L.Author
Easton, A. J.Author
Hutchison, R.Author
Year1977 (December)Volume41
Issue320
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_41/41-320-487.pdf+
DOIdoi:10.1180/minmag.1977.041.320.10Search in ResearchGate
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Mindat Ref. ID2824Long-form Identifiermindat:1:5:2824:4
GUID0
Full ReferenceGraham, A. L., Easton, A. J., Hutchison, R. (1977) The Mayo Belwa meteorite: a new enstatite achondrite fall. Mineralogical Magazine, 41 (320) 487-492 doi:10.1180/minmag.1977.041.320.10
Plain TextGraham, A. L., Easton, A. J., Hutchison, R. (1977) The Mayo Belwa meteorite: a new enstatite achondrite fall. Mineralogical Magazine, 41 (320) 487-492 doi:10.1180/minmag.1977.041.320.10
In(1977, December) Mineralogical Magazine Vol. 41 (320) Mineralogical Society
Abstract/NotesSummaryMayo Belwa, a highly shocked enstatite achondrite, fell during the evening of 3 August 1974 in the Adamawa District, NE. Nigeria (8° 58' N., 12° 05' E.). The stone weighed 4·85 kg and was deposited in the Geological Survey of Nigeria and loaned for study to the British Museum (Natural History). It is composed principally of enstatite (0·02 FeO%), with some olivine (Fo100), diopside, feldspar (An9 Ab88 Or3), and minor Fe-Ni metal and the sulphides oldhamite, daubréelite, ferroan alabandine, and troilite. The kamacite contains between 0·15% and 1·2% Si and the troilite contains 1·1% Ti. The meteorite possesses vuggy cavities, which contain fluor-amphibole needles projecting from their walls, suggesting the presence at some time of a volatile-rich phase. The titanium-rich troilite, the nearly ironfree enstatite and the Mg/Si ratio are typical of the E-achondrites.


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