Quantitative mapping of the oxidative effects of mantle metasomatism
The oxidation state of Fe in garnets in a garnet peridotite xenolith from the Wesselton kimberlite (South Africa) was quantitatively mapped using X-ray absorption near edge structure (XANES) spectroscopy. Maps of Fe3+/ΣFe were produced by recording the f
|Collections||ANU Research Publications|
|01_Berry_Quantitative_mapping_of_the_2013.pdf||946.58 kB||Adobe PDF||Request a copy|
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.