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Deep below Earth's surface lies a thick rocky layer called the mantle, which makes up the majority of our planet's volume. While Earth's mantle is too deep for humans to observe directly, certain mete...
Pure stishovite and coesite samples with zero porosity and dimensions appropriate for planar shock wave experiments have been synthesized with multi-anvil highpressure techniques. The equation of st...
OneclassofmodelsfortheearlyhistoryoftheEarthrequiresthepresent-dayinventory ofsiderophileelementsinthemantletohavebeenestablishedbyequilibriumpartitioning betweencore-formingmetalandmantlemineralsat...
ThefullelasticconstanttensoroforthorhombicMgSiO perovskitehasbeendetermined from?rstprinciplesforthe?rsttimeathighpressureusingtheplane-wavepseudopotential method.Theathermalelasticmoduli,determined...
First-principleslinear-response calculations wereusedto investigate the lattice dynamics ofwhatis thought to be the third mostabundant phase in the lower mantle,CaSi03 perovskite.Thecommonly assumed c...

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