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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 ...

    Jacob B. Forshaw, David R. M. Pattison in Contributions to Mineralogy and Petrology (2021)

  2. Article

    Open Access

    Preferred 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...

    Alexandra B. Nagurney, Mark J. Caddick, David R. M. Pattison in Scientific Reports (2021)

  3. No Access

    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...

    Paul G. Starr, David R. M. Pattison in Contributions to Mineralogy and Petrology (2019)