par Kalfoun, Florence;Merlet, Claude;Ionov, Dimitri 
Référence Mikrochimica acta, 139, 1-4, page (83-91)
Publication Publié, 2002
Référence Mikrochimica acta, 139, 1-4, page (83-91)
Publication Publié, 2002
Article révisé par les pairs
| Résumé : | Depletion of high field strength elements (HFSE: Nb, Ta, Zr, Hf) relative to other lithophile trace elements in arc magmas and variations of Nb/Ta and Zr/Hf ratios in mantle-derived rocks can be addressed through studies of minerals, which concentrate and fractionate these elements. The presence of rutile, a common accessory Ti-oxide phase in various mantle rocks, has often been invoked to explain the Nb and Ta depletion in arc lavas because it has the highest HFSE abundances among the known mantle minerals. In this study, we measure the concentrations of Nb, Ta, Zr and Hf (at > 200 ppm) in rutile of two metasomatized mantle lherzolites using a Cameca SX-100 electron microprobe and obtain Nb/Ta ratios with an accuracy of about ±5%. Mass balance calculations indicate that ≤1-5% of Nb and Ta in the rocks reside in major minerals and that the balance is hosted by accessory Tioxides. The Nb/Ta ratios vary signiicantly in nearby rutile grains in both peridotites (17-33, average 23; 12-37, average 21). Therefore, individual rutile grains may not be representative of the total grain population. However, Nb/Ta ratios measured in the bulk rock lherzolites by solution ICP-MS (21 ± 0.3) are within the analytical error of the average Nb/Ta values calculated for 5-7 rutile grains in both samples. These results emphasise that a representative grain selection must be analysed in order to determine trace elements contents of bulk rocks from data on accessory phases. © Springer-Verlag 2002. |
