Fig. 3: Change of magma ocean viscosity with depth.
From: Formation of bridgmanite-enriched layer at the top lower-mantle during magma ocean solidification
a, b We report MO viscosities with KLB-1 (left) and chondrite-type (right) compositions for potential surface temperatures from 2000 to 3000 K. Solid and dashed lines are calculated along mantle adiabats and liquidus profiles, respectively. c, d Solid and dashed lines represent adiabatic63 and liquidus55,56 profiles, respectively, for molten KLB-1 and chondrite-type mantle compositions.
