Crystal entrainment from cool, low-silica rocks into hot, high-silica melts: diverse primary melt compositions at Taranaki volcano, New Zealand
收藏资源简介:
Supplementary Data: <b>SD1:</b> Sample source, stratigraphical unit, location, age, TAS ID and type. <b>SD2:</b> Major oxide compositions, weight loss on ignition (LOI), and minor and trace element concentrations of the lavas of Taranaki from this study. <b>SD3:</b> Major oxide concentrations of samples from Taranaki from literature (Price <i>et al.</i> 1992, 1999; Stewart <i>et al.</i> 1996; R. B. Stewart pers. comm. 2018; Zernack <i>et al.</i> 2012). <b>SD4:</b> Minor and trace element concentrations of samples from Taranaki from literature (Price <i>et al.</i> 1992, 1999; Stewart <i>et al.</i> 1996; R. B. Stewart pers. comm. 2018; Zernack <i>et al.</i> 2012). <b>SD5:</b> EPMA spot analyses of mineral crystals from this study. <b>SD6:</b> Major oxide concentrations of groundmass of lavas of Taranaki, measured through defocussed EPMA beam. Average of 30 spot analyses used. <b>SD7:</b> Modal proportions of mineral phases, groundmass, and vesicles of lavas of Taranaki. <b>SD8:</b> Accuracy and precision for all analyses.



