Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
9451146 | Chemie der Erde - Geochemistry | 2005 | 18 Pages |
Abstract
The REE fractionation patterns in all three arfvedsonite granite varieties are characterized by enrichment of both the light (La-Sm) and heavy (Gd-Lu) rare earth elements and a significant negative Eu anomaly. The albite arfvedsonite granite is, however, preferentially more enriched in the heavy REE relative to the aegirine arfvedsonite and the arfvedsonite granites. A plot of the âREE against Na2O and niobium reveals positive correlation in the arfvedsonite granites. There is also a linear relationship and strongly positive correlation between Nb and Na2O because the pyrochlore is most abundant in the most extensively albitized variety of the arfvedsonite granites.
Keywords
Related Topics
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Geochemistry and Petrology
Authors
P.O. Ogunleye, E.C. Ike, I. Garba,