interior_lookup_tables/1TPa-dK09-elec-free/MgSiO3_Wolf_Bower_2018_400GPa

This high P–T EOS applies a generalized Rosenfeld–Tarazona model as a thermal perturbation to isothermal and adiabatic reference compression curves, resulting in a thermodynamically consistent formulation. RTpress remains accurate over a wide P-T range and depends on a limited number of physical parameters, which are calibrated from experimental or simulation data.

In this case, we use their parameterization for MgSiO₃ melt, representing a rocky mantle composition up to 400GPa. Mirror of Zenodo deposit 10.5281/zenodo.15877424. Zenodo is the primary source.