Fig. 6From: Sound velocities of bridgmanite from density of states determined by nuclear inelastic scattering and first-principles calculationsComparison of majorite and bridgmanite sample data at 0 GPa. a NIS spectra. b pDOS (upper) and reduced pDOS (lower). Majorite was measured as the starting material in air while bridgmanite samples were measured after decompressionBack to article page