The effect of silica activity on the diffusion of Ni and Co in olivine
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Zhukova, Irina
O'Neill, Hugh
Campbell, Ian
Kilburn, Matt R
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Springer
Abstract
The diffusion of Ni and Co was measured at atmospheric pressure in synthetic monocrystalline forsterite (Mg2SiO4) from 1,200 to 1,500 °C at the oxygen fugacity of air, along [100], with the activities of SiO2 and MgO defined by either forsterite + pericl
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Contributions to Mineralogy and Petrology
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2037-12-31