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).<br>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)<br><br>