Supplementary Table S1‒6 for "The effect of fluorine on mineral-carbonatitic melt partitioning of trace elements – Implications for critical mineral deposits"

Table S1. Calculated trace element concentrations of 0.03-0.3% carbonatitic melt from garnet lherzolite and spinel lherzolite under fluorine-bearing and fluorine-free conditions.Table S2. Calculated bulk Ds applicable for sediment and oceanic crust derived carbonatite.Table S3. Calculated trace element concentrations of 0.03-1% ocean crust derived carbonatite using newly obtained partition coefficients.Table S4. Calculated trace element concentrations of 0.03-1% sediment eclogite-derived carbonatite using newly obtained partition coefficients.Table S5. Trace element characteristics of continental lithospheric mantle with the addition of carbonatitic melt from subducted sediments and ocean crusts.Table S6. Calculated trace element concentrations of 0.03-1% carbonatitic melt from continental lithospheric mantle (garnet lherzolite) metasomatized by sediments and ocean crust derived carbonatitic melt under fluorine-bearing conditions.

表S1 含氟与无氟条件下，石榴石二辉橄榄岩及尖晶石二辉橄榄岩源0.03%~0.3%碳酸盐熔体的微量元素浓度计算结果
表S2 沉积物及洋壳来源碳酸盐岩适用的总分配系数（bulk Ds）计算结果
表S3 利用最新获取的分配系数计算得到的0.03%~1%洋壳来源碳酸盐岩的微量元素浓度
表S4 利用最新获取的分配系数计算得到的0.03%~1%沉积物源榴辉岩型碳酸盐岩的微量元素浓度
表S5 经俯冲沉积物与洋壳来源碳酸盐熔体交代后的大陆岩石圈地幔的微量元素特征
表S6 含氟条件下，经沉积物与洋壳来源碳酸盐熔体交代的大陆岩石圈地幔（石榴石二辉橄榄岩）所形成的0.03%~1%碳酸盐熔体的微量元素浓度计算结果