Extended Data Fig. 10: Rock physics modelling using the Voigt-Reuss-Hill (VRH) averaging.
From: Lower oceanic crust formed by in situ melt crystallization revealed by seismic layering
(a) Physical properties of Olivine (Ol), Clinopyroxene (Cpx) and Plagioclase (Pl) from [Sobolev and Babeyko 1994]. (b) The effective seismic P-wave velocities from Voigt-Reuss-Hill (VRH) averaging using different fraction volumes of mineral components (Ol, Cpx and Pl).
