Physics
Scientific paper
Dec 1992
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992pcmo.work...56t&link_type=abstract
In Lunar and Planetary Inst., Workshop on the Physics and Chemistry of Magma Oceans from 1 Bar to 4 Mbar p 56-57 (SEE N92-28587
Physics
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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