Fig. 7
From: A coupled core-mantle evolution: review and future prospects
Examples of the coupled core-mantle evolution in mantle convection simulations when inserting the formation of the stable region formulated by Nakagawa (2018). a Temperature at the CMB, b heat flow across the CMB, c inner core, d magnetic dissipation, and e thermal and chemical structure taken at t = 4.6 Gyrs. For the chemical structure, blue indicates the depleted harzburgite and red indicates the enriched oceanic crust