interior_lookup_tables/Melting_curves/Monteux+600

In Monteux et al. (2016), the solidus and liquidus profiles are obtained by fitting experimental data with a modified Simon–Glatzel equation (Simon & Glatzel, 1929). For pressures below 20 GPa, they use experimentally determined solidus and liquidus temperatures for a chondritic mantle composition from Herzberg and Zhang (1996). At pressures above 20 GPa, the difference between the F-peridotitic and A-chondritic solidus curves is considered negligible, and thus the A-chondritic solidus from Andrault et al. (2011) is adopted. The liquidus curves are fitted independently: the F-peridotitic liquidus follows Fiquet et al. (2010), while the A-chondritic liquidus is based on Andrault et al. (2011), each with their respective fitting parameters.In this case, this set of melting curves was created in such a way that the solidus (Equations (10,12) from Monteux et al. (2016)). is used a a normal solidus, and the liquidus is the solidus shifted +600K