Author: Martin Audrey M. Hammouda Tahar
Publisher: E. Schweizerbart'sche Verlagsbuchhandlung
ISSN: 0935-1221
Source: European Journal of Mineralogy, Vol.23, Iss.1, 2011-02, pp. : 5-16
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Abstract
We have investigated the effect of iron and oxygen fugacity on dolomite + coesite stability during subduction. For redox conditions buffered by the assemblage itself, the presence of iron (Fe/(Fe + Mg)
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