| Reference Type | Journal (article/letter/editorial) |
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| Title | The Pendennis peralkaline minette |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Hall, A. | Author |
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| Year | 1982 | Volume | 45 |
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| Issue | 337 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_45/45-337-257.pdf+ |
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| DOI | doi:10.1180/minmag.1982.045.337.29Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 3339 | Long-form Identifier | mindat:1:5:3339:2 |
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| GUID | 0 |
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| Full Reference | Hall, A. (1982) The Pendennis peralkaline minette. Mineralogical Magazine, 45 (337) 257-266 doi:10.1180/minmag.1982.045.337.29 |
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| Plain Text | Hall, A. (1982) The Pendennis peralkaline minette. Mineralogical Magazine, 45 (337) 257-266 doi:10.1180/minmag.1982.045.337.29 |
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| In | (1982) Mineralogical Magazine Vol. 45 (337) Mineralogical Society |
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| Abstract/Notes | AbstractThe Pendennis minette has an exceptionally high K2O/Na2O ratio and is strongly peralkaline. Its constituent minerals, which are described in detail, are sanidine, biotite, two carbonates (dolomite and ferroan magnesite), two amphiboles (riebeckite and a new variety, potassium magnesio-arfvedsonite), and quartz. The major and trace dement composition of the minette indicates close affinities with the lamproitic lavas. |
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