| Reference Type | Journal (article/letter/editorial) |
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| Title | Ocellar Hybrids from the Tyrone Igneous Series, Ireland |
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| Journal | Geological Magazine |
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| Authors | Angus, N. S. | Author |
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| Year | 1962 (February) | Volume | 99 |
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| Issue | 1 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800057071Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 249145 | Long-form Identifier | mindat:1:5:249145:9 |
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| GUID | 0 |
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| Full Reference | Angus, N. S. (1962) Ocellar Hybrids from the Tyrone Igneous Series, Ireland. Geological Magazine, 99 (1) 9-26 doi:10.1017/s0016756800057071 |
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| Plain Text | Angus, N. S. (1962) Ocellar Hybrids from the Tyrone Igneous Series, Ireland. Geological Magazine, 99 (1) 9-26 doi:10.1017/s0016756800057071 |
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| In | (1962, February) Geological Magazine Vol. 99 (1) Cambridge University Press (CUP) |
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| Abstract/Notes | AbstractOcellar hybrid rocks, formed by metasomatic transformation of basalt xenoliths engulfed in granitic magma, are characterized by numerous small, oval quartz porphyroblasts, each sheathed with narrow rims of amphibole. The progressive development of these quartz ocelli, together with the general texture of the ocellar hybrid, is traced through a number of intermediate hybrid types. In some instances, the ocellar hybrid displays an intrusive relationship toward basalt and is thought to have undergone a certain amount of metasomatic mobilization. |
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