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McCall, G. J. H., Cleverly, W. H. (1968) New stony meteorite finds including two ureilites from the Nullarbor Plain, Western Australia. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (281) 691-716 doi:10.1180/minmag.1968.036.281.12

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Reference TypeJournal (article/letter/editorial)
TitleNew stony meteorite finds including two ureilites from the Nullarbor Plain, Western Australia
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsMcCall, G. J. H.Author
Cleverly, W. H.Author
Year1968 (March)Volume36
Page(s)691-716Issue281
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_36/36-281-691.pdf+
DOIdoi:10.1180/minmag.1968.036.281.12Search in ResearchGate
Mindat Ref. ID6140Long-form Identifiermindat:1:5:6140:1
GUIDa1f7d6b2-f417-4ae0-bf3a-32624ecbfd81
Full ReferenceMcCall, G. J. H., Cleverly, W. H. (1968) New stony meteorite finds including two ureilites from the Nullarbor Plain, Western Australia. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (281) 691-716 doi:10.1180/minmag.1968.036.281.12
Plain TextMcCall, G. J. H., Cleverly, W. H. (1968) New stony meteorite finds including two ureilites from the Nullarbor Plain, Western Australia. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (281) 691-716 doi:10.1180/minmag.1968.036.281.12
In(1966) Mineralogical Magazine Vol. 36 (281) Mineralogical Society
Abstract/NotesSummaryTwo groups of meteorite finds in separate areas of the Nullarbor Plain are reported. It is suggested that the grouping is due to the fact that these are areas in which a family of rabbit trappers operates: these people have made most of the finds. There is, however, one shower of 71 small meteorites represented. Several arrivals on earth are represented by each group. The meteorites are described and it is shown that several distinct types are represented. Two quite different ureilites have been identified—only the fourth and fifth ever discovered in the world. Analyses are given for these rare carbonaceous achondrite meteorites. The remainder of the stones are olivine-hypersthene and olivine-bronzite chondrites. The whole question of the reason for the profusion of meteorite recoveries now being made on the Nullarbor Plain is briefly discussed.


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