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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 diffus...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2167873529

Pressure, temperature, water content, and oxygen fugacity dependence of the Mg grain-boundary diffusion coefficient in forsterite

About this item

Full title

Pressure, temperature, water content, and oxygen fugacity dependence of the Mg grain-boundary diffusion coefficient in forsterite

Publisher

Washington: Mineralogical Society of America

Journal title

The American mineralogist, 2018-09, Vol.103 (9), p.1354-1361

Language

English

Formats

Publication information

Publisher

Washington: Mineralogical Society of America

More information

Scope and Contents

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...

Alternative Titles

Full title

Pressure, temperature, water content, and oxygen fugacity dependence of the Mg grain-boundary diffusion coefficient in forsterite

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_journals_2167873529

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2167873529

Other Identifiers

ISSN

0003-004X

E-ISSN

1945-3027

DOI

10.2138/am-2018-6480

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