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Mason, R. A., Smith, J. V., Dawson, J. B., Treves, S. B. (1982) A reconnaissance of trace elements in anorthoclase megacrysts. Mineralogical Magazine, 46 (338) 7-11 doi:10.1180/minmag.1982.046.338.02

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Reference TypeJournal (article/letter/editorial)
TitleA reconnaissance of trace elements in anorthoclase megacrysts
JournalMineralogical MagazineISSN0026-461X
AuthorsMason, R. A.Author
Smith, J. V.Author
Dawson, J. B.Author
Treves, S. B.Author
Year1982 (March)Volume46
Issue338
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_46/46-338-7.pdf+
DOIdoi:10.1180/minmag.1982.046.338.02Search in ResearchGate
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Mindat Ref. ID3347Long-form Identifiermindat:1:5:3347:7
GUID0
Full ReferenceMason, R. A., Smith, J. V., Dawson, J. B., Treves, S. B. (1982) A reconnaissance of trace elements in anorthoclase megacrysts. Mineralogical Magazine, 46 (338) 7-11 doi:10.1180/minmag.1982.046.338.02
Plain TextMason, R. A., Smith, J. V., Dawson, J. B., Treves, S. B. (1982) A reconnaissance of trace elements in anorthoclase megacrysts. Mineralogical Magazine, 46 (338) 7-11 doi:10.1180/minmag.1982.046.338.02
In(1982, March) Mineralogical Magazine Vol. 46 (338) Mineralogical Society
Abstract/NotesAbstractMajor, minor, and trace elements were measured with electron and ion microprobes for eighteen anorthoclase megacrysts from five locations. Comparisons with concentration ranges tabulated by Smith (1974) show excellent agreement except for consistently lower values of Mg and B. The discrepancy for Mg probably reflects Mg-rich impurities contaminating samples analysed by bulk methods. The cause of the discrepancy for B is unknown and deserves further study. Samples from Mt. Erebus, Antarctica, contain glass inclusions from which the following crystal/liquid partition coefficients ensue: Mg, 0.008; P, 0.04; Ti, 0.08; Fe, 0.04; Ba, 5.2; Sr, 8; Rb, 0.27.


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