| Reference Type | Journal (article/letter/editorial) |
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| Title | Gahnite and columbite in an alkali-feldspar granite from New Zealand |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Tulloch, A. J. | Author |
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| Year | 1981 (September) | Volume | 44 |
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| Issue | 335 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_44/44-335-275.pdf+ |
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| DOI | doi:10.1180/minmag.1981.044.335.06Search in ResearchGate |
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| Generate Citation Formats |
| Mindat Ref. ID | 3271 | Long-form Identifier | mindat:1:5:3271:5 |
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| GUID | 0 |
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| Full Reference | Tulloch, A. J. (1981) Gahnite and columbite in an alkali-feldspar granite from New Zealand. Mineralogical Magazine, 44 (335) 275-278 doi:10.1180/minmag.1981.044.335.06 |
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| Plain Text | Tulloch, A. J. (1981) Gahnite and columbite in an alkali-feldspar granite from New Zealand. Mineralogical Magazine, 44 (335) 275-278 doi:10.1180/minmag.1981.044.335.06 |
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| In | (1981, September) Mineralogical Magazine Vol. 44 (335) Mineralogical Society |
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| Abstract/Notes | AbstractGahnite and columbite with compositions (Zn5.96Fe1.55Mg0.21Mn0.13)ÎŁ7.85Al16.09O32 and (Nb7.36Ta0.60Mn2.95Fe0.98Ti0.09)ÎŁ11.98O24 occur as accessory phases in a highly evolved garnetiferous muscovite alkalifeldspar granite. Both phases have developed as a result of a concentration of Zn, Nb, and Ta during the fmal stages of the fractional crystallization which led to the formation of the pluton, and the lack of a major mafic mineral such as biotite, in which these elements are normally camouflaged in granitoid rocks. |
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