Figure 1 | Scientific Reports

Figure 1

From: Non-traditional stable isotope behaviors in immiscible silica-melts in a mafic magma chamber

Figure 1

Schematic illustration of FeO and SiO2 compositional profile and diffusion-induced Fe isotope fractionation of interfacial melt during the convective growth of an ascending Si-melt.

57FeO or 54FeO line represents a hypothetical diffusional profile for the corresponding pure FeO isotope endmember. The thickness of the interfacial melt is exaggerated for illustration purpose. See text for details.

Back to article page