| Reference Type | Journal (article/letter/editorial) |
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| Title | Contributions to the Petrology of Barnavave, Carlingford, I.F.S.—2. An Occurrence of Quartz-bearing Syenite and its Xenoliths |
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| Journal | Geological Magazine |
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| Authors | Nockolds, S. R. | Author |
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| Year | 1937 (March) | Volume | 74 |
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| Issue | 3 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800088609 |
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| Generate Citation Formats |
| Mindat Ref. ID | 246765 | Long-form Identifier | mindat:1:5:246765:2 |
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| GUID | 0 |
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| Full Reference | Nockolds, S. R. (1937) Contributions to the Petrology of Barnavave, Carlingford, I.F.S.—2. An Occurrence of Quartz-bearing Syenite and its Xenoliths. Geological Magazine, 74 (3) 125-132 doi:10.1017/s0016756800088609 |
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| Plain Text | Nockolds, S. R. (1937) Contributions to the Petrology of Barnavave, Carlingford, I.F.S.—2. An Occurrence of Quartz-bearing Syenite and its Xenoliths. Geological Magazine, 74 (3) 125-132 doi:10.1017/s0016756800088609 |
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| In | (1937, March) Geological Magazine Vol. 74 (3) Cambridge University Press (CUP) |
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| Abstract/Notes | On the eastern side of Barnavave, at the immediate junction of the igneous mass with the surrounding limestone and about a quarter of a mile south of the fault which crosses the mountain, there is an isolated outcrop of a fine-grained, speckled rock which clearly invades the limestone at this point. The rock includes xenoliths broken from the limestone and also others of igneous origin.-and smaller dimensions. Microscopical examination proves the rock to be a syenite of unusual character which carries a small amount of quartz. It is possibly the rock referred to by Harker. |
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These are possibly similar items as determined by title/reference text matching only.