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Shock compression of liquid silicates to 125 GPa: The anorthite‐diopside join
Shock compression The anorthite‐diopside join
2014/4/8
We determined the equation of state (EOS) of three silicate liquid compositions by
shock compression of preheated samples up to 127 GPa. Diopside (Di; Ca2Mg2SiO6)
at 1773 K, anorthite (An; CaAl2Si2O...
EFFECTS OF THE CHANGES IN SLOPE OCCURRING ON LIQUIDUS AND SOLIDUS PATHS IN THE SYSTEM DIOPSIDE-ANORTHITE-ALBITEI
THE CHANGES IN SLOPE OCCURRING ON LIQUIDUS SOLIDUS PATHS IN THE SYSTEM DIOPSIDE-ANORTHITE-ALBITEI
2014/4/8
Liquidus and solidus paths in the system diopside-anorthite-albite exhibit changes in slope. When plagioclase crystallizes alone from a ternary liquid both paths are steeper than in the system anorthi...
TRENDS AND AFFINITIES OF BASALTIC MAGMAS AND PYROXENES AS ILLUSTRATED ON THE DIOPSIDE-OLIVINE-SILICA DIAGRAM
TRENDS AFFINITIES OF BASALTIC MAGMAS PYROXENES AS ILLUSTRATED ON THE DIOPSIDE-OLIVINE-SILICA DIAGRAM
2014/4/8
The major normative components of basalts can be accommodated in the tetrahedra plagioclase-diopside-olivine-silica or plagioclase-diopside-olivine-nepheline. Average compositions of magma batches fro...