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Article
Ferrous/ferric (Fe2+/Fe3+) partitioning among silicates in metapelites
Fe3+ and XFe3+, defined as Fe3+/(Fe2+ + Fe3+) on a molar basis, are now recognised as key parameters in phase equilibrium modelling. A hindrance is that it is only possible to routinely measure total Fe, and not ...
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Article
Open AccessPreferred orientations of garnet porphyroblasts reveal previously cryptic templating during nucleation
Electron back scattered diffraction data of garnet crystals from the Nelson Aureole, British Columbia and the Mosher’s Island formation, Nova Scotia, reveals that 22 garnet crystals are all oriented with one o...
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Article
Equilibrium and disequilibrium processes across the greenschist–amphibolite transition zone in metabasites
Documentation of textures, modes and compositions of minerals in metamorphosed basalts across two greenschist-to-lower amphibolite facies sequences (Flin Flon, Manitoba and Rossland, British Columbia) was comb...