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收藏DataCite Commons2024-06-11 更新2024-07-13 收录
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Supplementary Figure 2 Chemical composition of the Apollo 14 high-Al basalts and picritic glass beads outlined as colored areas (i.e., bordered with point-dashed; data sources: Delano, 1986; Shearer and Papike, 1993; Papike et al., 1997) compared to our experimental quenched melts (circles: KREEP-bearing and squares: KREEP-free starting materials). The light green area bordered by dashes depicts the compositions of low-Ti, high-Al mare basalts (Hallis et al. 2004, Fagan et al. 2014). The compositions of experimental quenched melts of Singletary and Grove (2008), denoted as SG08, are depicted in the turquoise triangle and surrounded by a dotted line. The grey arrows indicate the fractionation path upon drop of T in between experiments. (a) Mg# vs TiO2 and (b) SiO2 vs FeO
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2024-06-11
