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The solubility of heat-producing elements in Earth’s core

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Academic year: 2021

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Figure

Figure 1   Thermodynamic models of K and U partitioning between metal and silicate. (a) Equilibrium constant for potassium  metal-silicate partitioning (Eq
Figure 2   Concentration of K and U in the core from continuous core-formation models, assuming two magma ocean geotherms:

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