In this study, we model the core structure of screw dislocations with [1 0 0] and [0 1 0] Burgers vector in MgSiO 3 perovskite, in the pressure range of Earth's lower mantle (25-130 GPa).We use a generalized Peierls-Nabarro model, called Peierls-Nabarro-Galerkin, based on generalized stacking-fault energy calculations.These stacking-fault energy calculations are performed using a pairwise potential parametrization and compared to ab initio results.The results of Peierls-Nabarro-Galerkin calculations demonstrate that [1 0 0] dislocation and [0 1 0] are, respectively, characterized by a planar core spreading in (0 1 0) and (1 0 0).Our results emphasize the role of [1 0 0](0 1 0) and [0 1 0](1 0 0) slip systems in the deformation mechanism of MgSiO 3 perovskite.Furthermore, we validate the use of pairwise potential for further dislocation modelling of such minerals at the atomic scale.
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Gouriet et al. (2014) studied this question.
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