The importance of defining chemical potentials, substitution mechanisms and solubility in trace element diffusion studies: the case of Zr and Hf in olivine
Date
2014
Authors
Jollands, Michael
O'Neill, Hugh
Hermann, Joerg
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Springer
Abstract
The diffusion, substitution mechanism and solubility limits of Zr and Hf in synthetic forsterite (Mg2SiO4) and San Carlos olivine (Mg0.9Fe0.1)2SiO4 have been investigated between 1,200 and 1,500 °C as a function of the chemical potentials of the componen
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Contributions to Mineralogy and Petrology
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Journal article
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2037-12-31
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