How the core-mantle differentiation shaped volatile elements in the EarthEarth’s rocky layers are mysteriously low in nitrogen compared with carbon

Crystallographic preferred orientation of phase D at high pressure and temperature.Well-controlled uniaxial and simple shear deformation experiments

The lattice thermal conductivity (κlat) of lower mantle (LM) minerals is a key physical quantity for understanding the dynamics and thermal history o

The lattice thermal conductivity (κlat) of lower mantle (LM) minerals is a key physical quantity for understanding the dynamics and thermal history of

Velocities of aluminum enriched superhydrous phase B suggest the presence of hydrated mantle regions beneath subduction zonesResearchers at the Geod