Evidences for the terrestrial magma ocean from high-pressure melting experiments

Physics

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Earth Planetary Structure, Experimentation, High Pressure, Magma, Melting, Oceans, Planetary Evolution, Chondrites, Liquidus, Peridotite, Phase Diagrams, Solidus

Scientific paper

In order to study the early evolutionary history of our planet, the author has carried out a series of melting experiments on primitive mantle peridotites. Using a new multi-anvil apparatus (SPI-1000), the author revisited the melting study on mantle peridotites and also started a melting study for representative chondrite compositions in the pressure range of 25 Gpa. The updated phase diagram for the peridotite is shown as is the preliminary melting phase diagram for Allende C3 chondrite. The liquidus and solidus of the Allende chondrite are extrapolated based on experimental results at 24 to 26 GPa on the same rock.

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