| Reference Type | Journal (article/letter/editorial) |
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| Title | Olivine, pyroxene, feldspar, and spinel in ultramafic nodules from Auckland, New Zealand |
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| Journal | Mineralogical Magazine |
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| Authors | Rodgers, K. A. | Author |
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| Brothers, R. N. | Author |
| Year | 1969 (September) | Volume | 37 |
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| Issue | 287 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_37/37-287-375.pdf+ |
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| DOI | doi:10.1180/minmag.1969.037.287.11Search in ResearchGate |
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| Generate Citation Formats |
| Mindat Ref. ID | 6300 | Long-form Identifier | mindat:1:5:6300:9 |
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| GUID | 0 |
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| Full Reference | Rodgers, K. A., Brothers, R. N. (1969) Olivine, pyroxene, feldspar, and spinel in ultramafic nodules from Auckland, New Zealand. Mineralogical Magazine, 37 (287) 375-390 doi:10.1180/minmag.1969.037.287.11 |
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| Plain Text | Rodgers, K. A., Brothers, R. N. (1969) Olivine, pyroxene, feldspar, and spinel in ultramafic nodules from Auckland, New Zealand. Mineralogical Magazine, 37 (287) 375-390 doi:10.1180/minmag.1969.037.287.11 |
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| In | (1969, September) Mineralogical Magazine Vol. 37 (287) Mineralogical Society |
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| Abstract/Notes | SummaryChemical, optical, and X-ray data are presented for forsteritic olivine, bronzite-enstatite, diopsidic augite, anorthite, and spinel from ultramafic nodules at seven localities in Auckland province. Olivine has a composition range from Fo79–93 for large primary crystals to Fo80–100 for smaller interstitial grains. Orthopyroxenes (En83–96) carry exsolution lamellae of clinopyroxene parallel to (100); clinopyroxenes are mainly diopsidic augites with exsolved bronzite. The plagioclase (An97) has high-temperature characteristics and a lattice structure probably transitional between primitive and body-centred anorthite. Spinels include chromite, picotite, ceylonite, hercynite, and magnetite. Element distribution indicates that the ultramafic assemblages attained equilibrium at temperatures near 1250 °C and at moderate pressures, corresponding to the melting interval of anhydrous basaltic magmas within the uppermost mantle. |
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