Skip navigation
Skip navigation

An experimental determination of the effect of pressure on the Fe 3+ /ΣFe ratio of an anhydrous silicate melt to 3.0 GPa

O'Neill, Hugh; Berry, Andrew; McCammon, Catherine; Campbell, Stuart James; Jayasuriya, Kasthuri; Foran, Garry J


The effect of pressure on the Fe3+/∑Fe ratio of an anhydrous andesitic melt was determined from 0.4 to 3.0 GPa at 1400 °C with oxygen fugacity controlled internally by the Ru + RuO2 buffer. Values of Fe3+/∑Fe were determined by Mössbauer spectroscop

CollectionsANU Research Publications
Date published: 2006
Type: Journal article
Source: American Mineralogist
DOI: 10.2138/am.2005.1929


File Description SizeFormat Image
01_O'Neill_An_experimental_determination_2006.pdf255.42 kBAdobe PDF    Request a copy

Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.

Updated:  19 May 2020/ Responsible Officer:  University Librarian/ Page Contact:  Library Systems & Web Coordinator