Timescale and morphology of Martian mantle overturn immediately following magma ocean solidification

Keyphrases

• Viscosity 100%
• Magma Ocean 100%
• Thermal Convection 100%
• Martian Mantle 100%
• Mantle Overturn 100%
• Mars 50%
• Density Profile 50%
• Surface Material 50%
• Terrestrial Planets 50%
• As(III) 50%
• Temperature Effect 50%
• Layer Thickness 50%
• Entrainment 50%
• Silicate 50%
• Compositional Stability 50%
• Thermal Diffusion 50%
• Rayleigh-Taylor 50%
• Cumulate 50%
• Core Dynamo 50%
• Core-mantle Boundary 50%
• Silicate Magmas 50%
• Magma Ocean Crystallization 50%
• Dense Surface 50%
• Solidification Process 50%
• Viscosity Contrast 50%
• Isoviscous 50%
• Cumulate Overturn 50%
• Mantle Structure 50%

Earth and Planetary Sciences

• Magma 100%
• Silicate 66%
• Free Convection 66%
• Lithosphere 33%
• Terrestrial Planet 33%
• Core-Mantle Boundary 33%
• Harmonics 33%
• Thermal Diffusion 33%
• Mantle Structure 33%