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9.04 - Magma Oceans and Primordial Mantle Differentiation
V. Solomatov
Department of Earth & Planetary Sciences
Research output
:
Chapter in Book/Report/Conference proceeding
›
Chapter
›
peer-review
167
Scopus citations
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Keyphrases
Magma Ocean
100%
Primordial Mantle
100%
Mantle Differentiation
100%
Crystal-melt Segregation
100%
Crystal Growth
40%
Crystallization
40%
Chemical Differentiation
40%
Crystallite Size
40%
Geochemical Constraints
40%
Non-classical Crystallization
40%
Nucleation Growth
40%
Crystal Fractionation
40%
Order of Magnitude
20%
Creep
20%
Equilibrium Model
20%
Solid State
20%
Limited Time
20%
Physical Parameters
20%
Low Pressure
20%
Long Lifetime
20%
Liquid Phase
20%
Large Uncertainty
20%
Temperature Drop
20%
Early Earth
20%
Upper Mantle
20%
End-member Model
20%
Convective Heat Transfer
20%
Thermal Profile
20%
Planetary Evolution
20%
Mantle Convection
20%
Fractional Crystallization
20%
Partially Molten
20%
Molten Layer
20%
Liquidus
20%
Continuous Crystal
20%
Liquid Iron
20%
Convective Heating
20%
Convective Cooling
20%
Crystallization Differentiation
20%
Radiogenic Heating
20%
Melt Percolation
20%
Engineering
Convective
100%
Crystal Size
100%
Equilibrium Model
100%
Early Stage
50%
Liquid Phase
50%
Physical Parameter
50%
Creep
50%
Equilibrate
50%
Temperature Drop
50%
Heat Transport
50%
Liquid Iron
50%
Dissolution Cycle
50%
Earth and Planetary Sciences
Magma
100%
Nucleation
40%
Crystal Growth
40%
Equilibrium Model
40%
Early Earth
20%
Upper Mantle
20%
Liquid Phase
20%
Iron
20%
Mantle Convection
20%
Planetary Evolution
20%
Fractional Crystallization
20%
Percolation
20%
Material Science
Nucleation
100%
Crystal Growth
100%
Creep
50%
Percolation
50%
Surface (Surface Science)
50%