| Reference Type | Journal (article/letter/editorial) |
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| Title | Gahnite in the ∼3.75 Ga Isua Greenstone Belt, West Greenland |
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| Journal | Mineralogical Magazine |
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| Authors | Appel, P. W. U. | Author |
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| Year | 2000 (February) | Volume | 64 |
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| Issue | 1 |
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| Publisher | Mineralogical Society |
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| DOI | doi:10.1180/002646100549049Search in ResearchGate |
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| Generate Citation Formats |
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| Classification | Not set | LoC | Not set |
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| Mindat Ref. ID | 243135 | Long-form Identifier | mindat:1:5:243135:6 |
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| GUID | 0 |
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| Full Reference | Appel, P. W. U. (2000) Gahnite in the ∼3.75 Ga Isua Greenstone Belt, West Greenland. Mineralogical Magazine, 64 (1) 121-124 doi:10.1180/002646100549049 |
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| Plain Text | Appel, P. W. U. (2000) Gahnite in the ∼3.75 Ga Isua Greenstone Belt, West Greenland. Mineralogical Magazine, 64 (1) 121-124 doi:10.1180/002646100549049 |
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| Abstract/Notes | AbstractThe Zn-spinel gahnite has been discovered in the ∼3.75 Ga Isua Greenstone Belt, West Greenland. It is light blue-green to colourless in hand specimen and colourless in thin section as opposed to most other gahnites which are dark green to brown. The gahnites from Isua have very low Fe and Mg contents, and their compositions are thus close to the endmember gahnite. The gahnite was formed, during metamorphism, from sphalerite, in the absence of Fe-rich sulphides. |
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These are possibly similar items as determined by title/reference text matching only.
