| Reference Type | Journal (article/letter/editorial) |
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| Title | Hydrous cordierite with isotopically light oxygen from granulites, Strangways Range, Central Australia |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Wilson, Allan F. | Author |
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| Year | 1978 (March) | Volume | 42 |
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| Issue | 321 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_42/42-321-89.pdf+ |
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| DOI | doi:10.1180/minmag.1978.042.321.12Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 2863 | Long-form Identifier | mindat:1:5:2863:3 |
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| GUID | 0 |
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| Full Reference | Wilson, Allan F. (1978) Hydrous cordierite with isotopically light oxygen from granulites, Strangways Range, Central Australia. Mineralogical Magazine, 42 (321) 89-92 doi:10.1180/minmag.1978.042.321.12 |
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| Plain Text | Wilson, Allan F. (1978) Hydrous cordierite with isotopically light oxygen from granulites, Strangways Range, Central Australia. Mineralogical Magazine, 42 (321) 89-92 doi:10.1180/minmag.1978.042.321.12 |
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| In | (1978, March) Mineralogical Magazine Vol. 42 (321) Mineralogical Society |
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| Abstract/Notes | SummaryTwo new analyses of magnesian cordierites (MgO ∼ 12 %) reveal about 1% by weight of H2O +, and one sample contains 15 × 10−5 cm3STP/gm argon, which is twenty times in excess of argon expected for its age. Host granulites contain unexpectedly light oxygen, and three cordierites have δ 18O values of 2·0, 2·8, and 3·1 ‰, respectively. |
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