Anisotropy of Earth's D '' layer and stacking faults in the MgSiO3 post-perovskite phase

The post-perovskite phase of (Mg,Fe)SiO3 is believed to be the main mineral phase of the Earth’s lowermost mantle (the D 00 layer). Its properties explain1–6 numerous geophysical obser- vations associated with this layer — for example, the D 00 discon- tinuity7, its topography8 and seismic anisotropy within the layer9. Here we use a novel simulation technique, first-principles metadynamics, to identify a family of low-energy polytypic stacking-fault structures intermediate between the perovskite and post-perovskite phases. Metadynamics trajectories identify plane sliding involving the formation of stacking faults as the most favourable pathway for the phase transition, and as a likely mechanism for plastic deformation of perovskite and post- perovskite. In particular, the predicted slip planes are {010} for perovskite (consistent with experiment10,11) and {110} for post- perovskite (in contrast to the previously expected {010} slip planes1–4). Dominant slip planes define the lattice preferred orientation and elastic anisotropy of the texture. The {110} slip planes in post-perovskite require a much smaller degree of lattice preferred orientation to explain geophysical observations of shear-wave anisotropy in the D 00 layer.