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The effect of temperature on the equilibrium distribution of trace elements between clinopyroxene, orthopyroxene, olivine and spinel in upper mantle peridotite

✍ Scribed by Gudrun Witt-Eickschen; Hugh St.C. O'Neill


Book ID
116355508
Publisher
Elsevier Science
Year
2005
Tongue
English
Weight
701 KB
Volume
221
Category
Article
ISSN
0009-2541

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✍ Christopher J. Hatton πŸ“‚ Article πŸ“… 1984 πŸ› Springer 🌐 English βš– 982 KB

The coefficient for iron and magnesium exchange between olivine and liquid is modelled as a function of temperature in the simple system MgO -FeO-SiO2, and is found to be temperature insensitive in the range 1,200-1,400 ~ C, but temperature sensitive at higher temperatures. In natural systems silica