Calcium Isotope Fractionation in Plagioclase from Mafic-Ultramafic Rocks: Implications for Magmatic Processes and Planetary Differentiation

Here are a total of 10 tables. Table 1 shows the whole-rock major element compositions of the Panzhihua and Xiaohaizi intrusions; Table 2 presents the calcium isotope compositions of the whole-rock, clinopyroxene, and plagioclase in the two intrusions; Table 3 lists the Δ44/40CaPl-cpx values of samples in the two intrusions; Table 4 is the estimated Plagioclase-Melt Ca Fractionation Factors at 1273K; Table 5 is the estimated calcium isotopic composition of residual melts during the solidification of the lunar magma ocean;Table S1 shows the trace element data of clinopyroxene and plagioclase in the two intrusions; and Tables S2 to S5 respectively present the major element compositions of clinopyroxene and plagioclase in the Panzhihua and Xiaohaizi intrusions.本数据集共包含10张表格。表1展示了攀枝花（Panzhihua）与小海子（Xiaohaizi）侵入岩体的全岩主量元素组成；表2呈现了两处侵入岩体中全岩、单斜辉石（clinopyroxene）与斜长石（plagioclase）的钙同位素组成；表3列出了两处侵入岩体中各样品的Δ44/40CaPl-cpx值；表4为1273K条件下估算得到的斜长石-熔体钙分馏因子；表5为月球岩浆洋固结过程中残余熔体的钙同位素组成估算结果；附表S1展示了两处侵入岩体中单斜辉石与斜长石的微量元素数据；附表S2至S5则分别呈现了攀枝花与小海子侵入岩体中单斜辉石和斜长石的主量元素组成。