| Reference Type | Journal (article/letter/editorial) |
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| Title | Spinels from the Dawros Peridotite,
Connemara, Ireland |
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| Journal | Mineralogical Magazine |
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| Authors | Rothstein, A. T. V. | Author |
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| Year | 1972 (December) | Volume | 38 |
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| Issue | 300 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_38/38-300-957.pdf+ |
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| DOI | doi:10.1180/minmag.1972.038.300.06Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 6612 | Long-form Identifier | mindat:1:5:6612:3 |
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| GUID | 0 |
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| Full Reference | Rothstein, A. T. V. (1972) Spinels from the Dawros Peridotite,
Connemara, Ireland. Mineralogical Magazine, 38 (300) 957-960 doi:10.1180/minmag.1972.038.300.06 |
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| Plain Text | Rothstein, A. T. V. (1972) Spinels from the Dawros Peridotite,
Connemara, Ireland. Mineralogical Magazine, 38 (300) 957-960 doi:10.1180/minmag.1972.038.300.06 |
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| In | (1972, December) Mineralogical Magazine Vol. 38 (300) Mineralogical Society |
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| Abstract/Notes | SummaryTwo different spinels, analyses of which are given, occur in the layered ultramafic rocks at Dawros. Chrome spinel occurs both as gravity-stratified cumulates and as complex orbs, while an Al-rich spinel is both in rocks of the main Dawros magmatic sequence and in an association with an aluminous bronzite, which may originate by recrystallization. It is concluded that while the chrome spinel is certainly of magmatic origin, the aluminous spinel is probably partly of magmatic and partly of recrystallization origin. |
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