| Reference Type | Journal (article/letter/editorial) |
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| Title | The mineral chemistry of dolerites and gabbros from the central Complex of Slieve Gullion, NE Ireland |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Gamble, John A. | Author |
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| Year | 1982 (March) | Volume | 46 |
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| Issue | 338 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_46/46-338-103.pdf+ |
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| DOI | doi:10.1180/minmag.1982.046.338.16Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 3361 | Long-form Identifier | mindat:1:5:3361:3 |
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| GUID | 0 |
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| Full Reference | Gamble, John A. (1982) The mineral chemistry of dolerites and gabbros from the central Complex of Slieve Gullion, NE Ireland. Mineralogical Magazine, 46 (338) 103-110 doi:10.1180/minmag.1982.046.338.16 |
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| Plain Text | Gamble, John A. (1982) The mineral chemistry of dolerites and gabbros from the central Complex of Slieve Gullion, NE Ireland. Mineralogical Magazine, 46 (338) 103-110 doi:10.1180/minmag.1982.046.338.16 |
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| In | (1982, March) Mineralogical Magazine Vol. 46 (338) Mineralogical Society |
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| Abstract/Notes | SynopsisThe dolerites and gabbros of the Tertiary central complex of Slieve Gullion, NE Ireland, represent a suite of tholeiitic magmas (varying from tholeiitic basalt to tholeiitic andesite, Gamble 1979a) which crystallized in the root-zone of a shield volcano. The ubiquity of biotite suggests that the magmas were hydrous and, in addition, both silicate (olivine) and oxide (Ti-magnetite) phases show evidence for oxidation at high temperatures. |
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