Thermal structure of a vanishing subduction system. An example of seismically-derived crustal temperature along the Italian peninsula

This file contains the the temperature at the Moho, obtained from shear wave velocities (Molinari et al., 2015) and thermodynamic modeling, assuming a 3-layers crustal composition from Rudnick and Gao (2003).The .mat file that can be imported in Matlab or Octave and ready for plotting as it contains already gridded data.es. pcolor(lon, lat, mohodepth)