Solid-State Mantle Convection Coupled with a Crystallising Basal Magma Ocean

Learn about the complex interactions between solid-state mantle convection and crystallizing basal magma oceans in this 48-minute conference talk by Stephane Labrosse from the University of Lyon. Explore the fundamental processes that govern how Earth's mantle convects while coupled with a crystallizing magma ocean at its base, examining the thermal and chemical dynamics that influence planetary evolution. Discover the latest research on how these coupled systems affect heat transfer, chemical differentiation, and the long-term evolution of planetary interiors. Gain insights into the computational models and theoretical frameworks used to understand these complex geophysical processes, including the role of phase transitions, compositional variations, and thermal boundary layers in shaping mantle dynamics. Understand how basal magma ocean crystallization influences convection patterns, temperature distributions, and the formation of chemical heterogeneities that persist throughout geological time scales.