Extended Data Fig. 8: High-resolution geodynamic modelling results of the solidified BECMO with a higher Rayleigh number.
From: Deep mantle heterogeneities formed through a basal magma ocean contaminated by core exsolution

a–f, Snapshots of the temperature field (a,c,e) and the residual buoyancy field (b,d,f) of the geodynamic model. The parameters of this case are the same as those of the reference BECMO case, except for a Rayleigh number that is 5 times higher (5 × 107).