| Reference Type | Journal (article/letter/editorial) |
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| Title | Serpentinites in the North-East Ox Mountains, Eire |
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| Journal | Geological Magazine |
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| Authors | Lemon, G. G. | Author |
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| Year | 1966 (April) | Volume | 103 |
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| Issue | 2 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800050512Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 249609 | Long-form Identifier | mindat:1:5:249609:6 |
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| GUID | 0 |
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| Full Reference | Lemon, G. G. (1966) Serpentinites in the North-East Ox Mountains, Eire. Geological Magazine, 103 (2) 124-137 doi:10.1017/s0016756800050512 |
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| Plain Text | Lemon, G. G. (1966) Serpentinites in the North-East Ox Mountains, Eire. Geological Magazine, 103 (2) 124-137 doi:10.1017/s0016756800050512 |
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| In | (1966, April) Geological Magazine Vol. 103 (2) Cambridge University Press (CUP) |
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| Abstract/Notes | AbstractSix serpentinites occur in the Moinian granulites of the North-East Ox Mountains. Four have been known for some time and have been previously described. Additional information on these and the associated vermiculite deposits is provided. The remaining two serpentinites are described for the first time. A pyroxenite vein associated with one of these may have been produced by meta-morphic regeneration.The relationship of some of these serpentinites to the probable position of the Highland Boundary Fracture-zone in Eire is also discussed. Brief comparison is made with serpentinites occurring in the Scottish Moinian. |
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