Supplemental Material: Targeted P–T modelling and in-situ garnet dating on polymetamorphic metapelite provides the first compelling evidence for Rodinian tectonism recorded in south-west Tasmania

<p dir="ltr"><b>Supplementary material for Brown (2024), PhD thesis - Chapter 7 - </b><b>Targeted P–T modelling and in-situ garnet dating on polymetamorphic metapelite provides the first compelling evidence for Rodinian tectonism recorded in south-west Tasmania</b></p><p dir="ltr">Extended methods.</p><p dir="ltr"><b>Figure S1.</b> Modelled mineral modal proportions and compositions for the <i>P–T</i> pseudosections presented in Figure 7.9. Each isopleth marked pink represents the independently-calculated mode or composition of a given mineral.</p><p dir="ltr"><b>Table S1.</b> Representative EPMA results for solid solution minerals. Major element oxide compositions are given in wt%. Calculated mineral modal proportions in vol%. End-member proportions and selected oxide compositions for solid-solution minerals.</p><p dir="ltr"><b>Table S2.</b> Ti-in-quartz thermometry results. Ti (ppm) concentrations acquired using EPMA. Temperatures calculated using the calibration of Osborne et al. (2022).</p><p dir="ltr"><b>Table S3.</b> Additional details for laser-ablation and ICP–MS instruments used in this study.</p><p dir="ltr"><b>Table S4.</b> LA–ICP–MS/MS Lu–Hf isotope results for garnet. Major and trace-element data for a small selection of isotopes is provided. Data is also provided for primary reference material NIST-610, 'pseudo-primary' reference material Hogsbo, and secondary reference material Black Point.</p>