| Reference Type | Journal (article/letter/editorial) |
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| Title | The origin of accessory garnet in the Donegal Granite |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Hall, Anthony | Author |
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| Tyler, R. C. | Author |
| Year | 1965 (December) | Volume | 35 |
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| Issue | 272 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_35/35-272-628.pdf+ |
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| DOI | doi:10.1180/minmag.1965.035.272.06Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 5929 | Long-form Identifier | mindat:1:5:5929:3 |
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| GUID | 0 |
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| Full Reference | Hall, Anthony, Tyler, R. C. (1965) The origin of accessory garnet in the Donegal Granite. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (272) 628-633 doi:10.1180/minmag.1965.035.272.06 |
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| Plain Text | Hall, Anthony, Tyler, R. C. (1965) The origin of accessory garnet in the Donegal Granite. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (272) 628-633 doi:10.1180/minmag.1965.035.272.06 |
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| In | (1965) Mineralogical Magazine Vol. 35 (272) Mineralogical Society |
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| Abstract/Notes | SummaryIn the Donegal Granite garnet occurs as an accessory mineral in muscovite-granties, pegmatites, and aplites. The composition of the garnet in fourteen samples of granitic rock has been determined from the physical properties and three new chemical analyses are given. All the samples examined are intermediate in composition between almandine and spessartine. The reason for the high manganese content in garnet from granites is discussed. |
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