Publications des scientifiques de l'IRD

Dalou C., Koga K. T., Hammouda T., Poitrasson Franck. (2009). Trace element partitioning between carbonatitic melts and mantle transition zone minerals : implications for the source of carbonatites. Geochimica et Cosmochimica Acta, 73 (1), p. 239-255. ISSN 0016-7037.

Titre du document
Trace element partitioning between carbonatitic melts and mantle transition zone minerals : implications for the source of carbonatites
Année de publication
2009
Type de document
Article référencé dans le Web of Science WOS:000261914500015
Auteurs
Dalou C., Koga K. T., Hammouda T., Poitrasson Franck
Source
Geochimica et Cosmochimica Acta, 2009, 73 (1), p. 239-255 ISSN 0016-7037
The occurrence of CO2-rich lavas (carbonatites, kimberlites) and carbonate-rich xenoliths provide evidence for the existence of carbonatitic melts in the mantle. To model the chemical composition of such melts in the deep mantle, we experimentally determined partition coefficients for 23 trace elements (including REE, U-Th, HFSE, LILE) between deep mantle minerals and carbonatite liquids at 20 and 25 GPa and 1600 degrees C. Under these conditions, majoritic garnet and CaSiO3 perovskite are the main reservoirs for trace elements. This study used both femtosecond LA-ICP-MS and SIMS techniques to measure reliable trace element concentrations. Comparison of the two techniques shows a general agreement, except for Sc and Ba. Our experimentally determined partition coefficients are consistent with the lattice strain model. The data suggest an effect of melt structure on partition coefficients in this pressure range. For instance, strain-free partition coefficient (D-0) for majorite-carbonatite melts do not follow the order of cation valence, D-0(2+) > D-0(3+) > D-0(4+) observed for majorite-CO2-free silicate melts. The newly determined partition coefficients were combined with trace element composition of majoritic garnets found as inclusions in diamond to model trace element patterns of deep-seated carbonatites. The result compares favorably with natural carbonatites. This suggests that carbonatites can originate from the mantle transition zone.
Plan de classement
Géologie et formations superficielles [064]
Localisation
Fonds IRD [F B010053048]
Identifiant IRD
fdi:010053048
Contact