Kerr, A. (1981) Zoning in garnets from the mainland Lewisian. Mineralogical Magazine, 44 (334) 191-194 doi:10.1180/minmag.1981.044.334.12
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Zoning in garnets from the mainland Lewisian | ||
| Journal | Mineralogical Magazine | ISSN | 0026-461X |
| Authors | Kerr, A. | Author | |
| Year | 1981 (June) | Volume | 44 |
| Issue | 334 | ||
| Publisher | Mineralogical Society | ||
| Download URL | https://rruff.info/doclib/MinMag/Volume_44/44-334-191.pdf+ | ||
| DOI | doi:10.1180/minmag.1981.044.334.12Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 3251 | Long-form Identifier | mindat:1:5:3251:7 |
| GUID | 0 | ||
| Full Reference | Kerr, A. (1981) Zoning in garnets from the mainland Lewisian. Mineralogical Magazine, 44 (334) 191-194 doi:10.1180/minmag.1981.044.334.12 | ||
| Plain Text | Kerr, A. (1981) Zoning in garnets from the mainland Lewisian. Mineralogical Magazine, 44 (334) 191-194 doi:10.1180/minmag.1981.044.334.12 | ||
| In | (1981, June) Mineralogical Magazine Vol. 44 (334) Mineralogical Society | ||
| Abstract/Notes | AbstractTwo types of zoning are found in garnets from Lewisian rocks. One is due to retrogression of an earlier homogeneous garnet while the other results from growth (or equilibration) during falling temperatures. Both zoning patterns result from metamorphism during or after the Dionard tectonic phase of the Laxfordian event. | ||
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