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            <gco:CharacterString>Nitrogen contents and isotope values were measured on whole-rock and mineral-separate powders (biotite, Kspar, plagioclase, quartz) on a Thermo Fisher Scientific MAT253 Isotope Ratio Mass Spectrometer at the University of St Andrews. Oxygen isotopes were obtained at the Scottish Universities Environmental Research Centre (SUERC) stable isotope laboratory. Samples were analysed for major and trace element composition by energy-dispersive X-ray fluorescence (ED-XRF) on a SPECTRO XEPOS HE spectrometer at the University of St Andrews In-situ major element data for biotite, Kspar, and plagioclase mineral phases were measured using the Cameca SX100 Electron Probe Micro Analyser (EPMA) in the Department of Earth Sciences at the University of Cambridge. In-situ trace element data for biotite, Kspar and plagioclase were measured in the Advanced Mass Spectrometry Lab of the Earth Observatory at the University of the Witwatersrand. This work is published in a peer-reviewed journal: Boocock, TJ., Stüeken, ES., Bybee, GM., König, R., Boyce, AJ., Prytulak, J., Buisman, I., Mikhail, S. 2023. Equilibrium partitioning and isotopic fractionation of nitrogen between biotite, plagioclase, and K-feldspar during magmatic differentiation. Geochimica et Cosmochimica Acta, 356, 116-128</gco:CharacterString>
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