Comparison between magma ocean and magma sill models. Magma ocean stages are indicated in yellow. "H3" describes the heating value below which radioactive heating from aluminum-26 is inefficient.
Shown are various parameters for both models, from left to right: melt fraction, temperature, radiogenic heating, melt/liquid upwelling velocity, composition fraction of liquid, and composition fraction of solid.
The composition is broken-down into the defined pseudo-components fsp, pxn, and olv. The model is started (= planetesimal formation time) at 0.9 Myr after CAIs.