First study of how volume percent of (Mg, Fe)O analog, NaCl, affects deformation and CPO in lower mantle analog assemblage.
Weaker NaCl controls rheology at 15% volume.
CPO in bridgmanite analog, NaMgF3, drastically reduced with 15% volume of NaCl.
NaCl does not acquire any notable CPO.
Results imply a weaker lower mantle and may explain why lower mantle is mostly isotropic.