Fig. A.3
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Thermal structure of the silicate atmosphere calculated by ATMO for different equilibrium temperatures Teq (indicated by the colors), which translates as different orbital radii. The dash-dotted PT profiles use the vapor computed via LavAtmos, while the plain lines use MAGMAVOL. The dashed line show the vapor pressure Pvap(T) corresponding to the limit between the magma ocean and the gaseous atmosphere.
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