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Campbell, I. H., Arndt, N. T. (1982) Pyroxene accumulation in spinifex-textured rocks. Geological Magazine, 119 (6) 605-610 doi:10.1017/s0016756800027096

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Reference TypeJournal (article/letter/editorial)
TitlePyroxene accumulation in spinifex-textured rocks
JournalGeological Magazine
AuthorsCampbell, I. H.Author
Arndt, N. T.Author
Year1982 (November)Volume119
Issue6
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800027096Search in ResearchGate
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Mindat Ref. ID252148Long-form Identifiermindat:1:5:252148:4
GUID0
Full ReferenceCampbell, I. H., Arndt, N. T. (1982) Pyroxene accumulation in spinifex-textured rocks. Geological Magazine, 119 (6) 605-610 doi:10.1017/s0016756800027096
Plain TextCampbell, I. H., Arndt, N. T. (1982) Pyroxene accumulation in spinifex-textured rocks. Geological Magazine, 119 (6) 605-610 doi:10.1017/s0016756800027096
In(1982, November) Geological Magazine Vol. 119 (6) Cambridge University Press (CUP)
Abstract/NotesSummaryNatural pyroxene spinifex-textured rocks, free of olivine, may have MgO contents as high as 15%. If these rocks are allowed to crystallize in the laboratory under equilibrium conditions, olivine is the liquidus phase at 1350°C and pyroxene does not appear until the temperature has fallen to 1180°C. A similar problem is encountered in high MgO komatiites. If spinifex-textured and aphyric komatiites from Munro Township are plotted on an MgO-CaO-Al2O3 diagram, olivine control is evident until the MgO content of the melt falls to 15%. At this point the liquid trend moves away from the CaO-MgO boundary, indicating the crystallization of pyroxene. If a high MgO komatiite is crystallized in the laboratory under equilibrium conditions, pyroxene does not appear until the MgO content of the liquid reaches 9%. It is suggested that experimental and natural systems behave differently because pyroxene has crystallized metastably in the natural system under conditions of extreme supercooling. The early metastable crystallization of pyroxene can only affect the liquid trend if the spinifex zone contains a cumulate component.


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