| Reference Type | Journal (article/letter/editorial) |
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| Title | Kornerupine in metasomatic zones, Strangways Range, Central Australia |
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| Journal | Mineralogical Magazine |
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| Authors | Woodford, P. J. | Author |
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| Wilson, Allan F. | Author |
| Year | 1976 (June) | Volume | 40 |
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| Page(s) | 589-594 | Issue | 314 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_40/40-314-589.pdf+ |
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| DOI | doi:10.1180/minmag.1976.040.314.05Search in ResearchGate |
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| Generate Citation Formats |
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| Classification | Not set | LoC | Not set |
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| Mindat Ref. ID | 6938 | Long-form Identifier | mindat:1:5:6938:4 |
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| GUID | 0 |
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| Full Reference | Woodford, P. J., Wilson, Allan F. (1976) Kornerupine in metasomatic zones, Strangways Range, Central Australia. Mineralogical Magazine, 40 (314). 589-594 doi:10.1180/minmag.1976.040.314.05 |
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| Plain Text | Woodford, P. J., Wilson, Allan F. (1976) Kornerupine in metasomatic zones, Strangways Range, Central Australia. Mineralogical Magazine, 40 (314). 589-594 doi:10.1180/minmag.1976.040.314.05 |
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| In | (1976, June) Mineralogical Magazine Vol. 40 (314) Mineralogical Society |
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| Abstract/Notes | SummaryThe first known occurrence of kornerupine in Australia is described. The mineral is a minor component of a phlogopite-rich garnet-corundum-spinel metasomatic zone, which cuts mafic and ultranlafic spinel-plagioclase-orthopyroxene-hornblende rocks. The kornerupine-bearing assemblage was formed during the second major metamorphic episode that affected the terrain, probably under low-grade granulite or upper amphibolite facies conditions. Kornerupine appears to have formed at significantly lower levels of P-T than those reached in the terrain during the peak of the second granulite metamorphism. |
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