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

✍ Scribed by Alain Perruchot


Book ID
104745499
Publisher
Springer
Year
1973
Tongue
English
Weight
344 KB
Volume
42
Category
Article
ISSN
0010-7999

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✦ Synopsis


When niekeliferous 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~ and 1 kbar), in favour of brueite.


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