Pressure, temperature, water content, and oxygen fugacity dependence of the Mg grain-boundary diffus...
Pressure, temperature, water content, and oxygen fugacity dependence of the Mg grain-boundary diffusion coefficient in forsterite
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Washington: Mineralogical Society of America
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Language
English
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Washington: Mineralogical Society of America
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Contents
The Mg grain boundary diffusion coefficients were measured in forsterite aggregates as a function of pressure (1 atm and 13 GPa), temperature (1100-1300 K), water content (<1-350 wt. ppm bulk water), and oxygen fugacity (10-18-10-0.7 bar) using a multi-anvil apparatus and a gas-mixing furnace. The diffusion profiles were analyzed by secondary ion m...
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Full title
Pressure, temperature, water content, and oxygen fugacity dependence of the Mg grain-boundary diffusion coefficient in forsterite
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TN_cdi_proquest_journals_2167873529
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2167873529
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ISSN
0003-004X
E-ISSN
1945-3027
DOI
10.2138/am-2018-6480