| Reference Type | Journal (article/letter/editorial) |
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| Title | The Granitic Cotectic Curve |
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| Journal | Geological Magazine |
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| Authors | Nockolds, S. R. | Author |
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| Year | 1947 (February) | Volume | 84 |
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| Page(s) | 19-28 | Issue | 1 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800082182 |
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| Mindat Ref. ID | 247600 | Long-form Identifier | mindat:1:5:247600:5 |
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| GUID | 210ad821-b98f-4c3b-bb2e-e2b0c6874997 |
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| Full Reference | Nockolds, S. R. (1947) The Granitic Cotectic Curve. Geological Magazine, 84 (1) 19-28 doi:10.1017/s0016756800082182 |
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| Plain Text | Nockolds, S. R. (1947) The Granitic Cotectic Curve. Geological Magazine, 84 (1) 19-28 doi:10.1017/s0016756800082182 |
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| In | (1947, February) Geological Magazine Vol. 84 (1) Cambridge University Press (CUP) |
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| Abstract/Notes | In a recent paper (Nockolds, 1946) it was shown that certain granite-aplites associated with acid plutonic rocks of Caledonian age in Western Scotland fell on, or were very close to, the plagioclase-potash felspar-quartz cotectic curve (the granitic cotectic curve), the approximate position of which could be determined from experimental data now available. It seemed of interest to determine whether other granite-aplites from other areas behaved in the same way and chemical analyses of granite-aplites and related rocks were collected from the literature with this end in view. |
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