| Reference Type | Journal (article/letter/editorial) |
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| Title | Garnets from the Eilat area, southern Israel |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Nathan, Y. | Author |
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| Katz, A. | Author |
| Eyal, M. | Author |
| Year | 1965 (June) | Volume | 35 |
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| Issue | 270 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_35/35-270-386.pdf+ |
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| DOI | doi:10.1180/minmag.1965.035.270.12Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 5881 | Long-form Identifier | mindat:1:5:5881:4 |
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| GUID | 0 |
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| Full Reference | Nathan, Y., Katz, A., Eyal, M. (1965) Garnets from the Eilat area, southern Israel. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (270) 386-392 doi:10.1180/minmag.1965.035.270.12 |
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| Plain Text | Nathan, Y., Katz, A., Eyal, M. (1965) Garnets from the Eilat area, southern Israel. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (270) 386-392 doi:10.1180/minmag.1965.035.270.12 |
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| In | (1965) Mineralogical Magazine Vol. 35 (270) Mineralogical Society |
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| Abstract/Notes | SummaryGarnets from twenty-eight pegmatites, schists, and gneisses from the crystalline massif of Eilat have been examined. Refractive index, unit-cell edge, MnO and FeO content were determined in 19 samples. Three chemical analyses are given. The garnets fall into two distinct groups, the pegmatite garnets (spessartine-rich, almandine to spessartine) and metamorphic garnets (nearly pure almandine). Garnets occurring in pegmatite-like granitoid veins cutting through the schists are shown to belong to the second (metamorphic) group. The pegmatite garnets again fall into two groups of different spessartine content. |
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