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Partage du nickel entre serpentine et brucite au cours de la serpentinisation du péridot

Partition of nickel between serpentine and brucite during serpentinisation of peridot

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Abstract

When nickeliferous peridot is submitted to a serpentinisation reaction with formation of brucite, the peridotic nickel is partitioned between the two minerals (serpentine and brucite) with a distribution coefficient K=[(Ni/Mg) brucite]/[(Ni/Mg)] serpentine=1,63 (at 350°C and 1 kbar), in favour of brucite.

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Bibliographie

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Authors and Affiliations

  1. Centre de Recherches sur la Synthèse et la Chimie des Minéraux, Rue de la Férollerie, 45045, Orléans-Cédex, France

    Alain Perruchot

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  1. Alain Perruchot
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Perruchot, A. Partage du nickel entre serpentine et brucite au cours de la serpentinisation du péridot. Contr. Mineral. and Petrol. 42, 229–234 (1973). https://doi.org/10.1007/BF00371587

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  • DOI: https://doi.org/10.1007/BF00371587

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