Fig. 4 | Nature Communications

Fig. 4

From: Immiscible hydrous Fe–Ca–P melt and the origin of iron oxide-apatite ore deposits

Fig. 4

Compositions of conjugate immiscible melts in this study compared to previous experimental melt pairs in tholeiitic systems19, 21,22,23,24,25,26 and native iron-hosted melt inclusions in lavas of the Siberian Traps27. DSi, the partitioning of SiO2 between the Fe-rich and Si-rich melts, expresses the compositional gap between the two melts, plotted as a function of elements partitioned into the Fe-rich melts

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