“…In particular the presence of atypical phases in primitive mantle, such as amphibole, phlogopite, carbonates, Ti minerals and others ("modal metasomatism";Harte, 1983) attests to the former presence of fluids or melts that significantly affected the mantle lithosphere and possibly changed its thermophysical properties, such as density and seismic velocity (Afonso and Schutt, 2012;Selway et al, 2015;Rader et al, 2015). In addition, peridotite fabric generates anisotropy and therefore affects the seismic response of the mantle (Savage, 1999).…”