| Reference Type | Journal (article/letter/editorial) |
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| Title | Cr Mica from the Precambrian Erris Complex, NW Mayo, Ireland |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Max, Michael D. | Author |
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| Treloar, P. J. | Author |
| Winchester, J. A. | Author |
| Oppenheim, M. J. | Author |
| Year | 1983 (September) | Volume | 47 |
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| Issue | 344 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_47/47-344-359.pdf+ |
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| DOI | doi:10.1180/minmag.1983.047.344.11Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 3530 | Long-form Identifier | mindat:1:5:3530:3 |
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| GUID | 0 |
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| Full Reference | Max, Michael D., Treloar, P. J., Winchester, J. A., Oppenheim, M. J. (1983) Cr Mica from the Precambrian Erris Complex, NW Mayo, Ireland. Mineralogical Magazine, 47 (344) 359-364 doi:10.1180/minmag.1983.047.344.11 |
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| Plain Text | Max, Michael D., Treloar, P. J., Winchester, J. A., Oppenheim, M. J. (1983) Cr Mica from the Precambrian Erris Complex, NW Mayo, Ireland. Mineralogical Magazine, 47 (344) 359-364 doi:10.1180/minmag.1983.047.344.11 |
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| In | (1983, September) Mineralogical Magazine Vol. 47 (344) Mineralogical Society |
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| Abstract/Notes | AbstractCr micas identified as chrome phengites occur in association with other Cr-rich minerals in a peculiar schist which lies along a complex shear zone within the pre-Caledonian Erris Complex. The schist generally has a chaotic internal structure but locally there is a crude planar mineralogical zoning with a serpentinebearing zone structurally above a Cr mica zone. Chemical analyses indicate that the schist is a tectonic derivative of a mixture of rock with a pronounced metasomatic character. |
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