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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...
Hydrogen in diopside: Diffusion, kinetics of extraction-incorporation, and solubility
Hydrogen diopside Diffusion kinetics extraction-incorporation solubility
2012/4/1
The kinetic of H extraction-incorporation in diopside single-crystals (Ca . Na Cr Mg0 97 0.02 0.01 0.97Fe Si O ) deduced by monitoring OH infrared absorption bands for samples heated from 973 to0.036 ...
Experimental study of the system phlogopite-diopside from 3.5 to 17 GPa
Experimental study system phlogopite-diopside 3.5 to 17 GPa
2012/4/6
Onthebasisofbothnaturalsamplesandexperimentalstudies,clinopyroxeneisapo-tentialreservoirforpotassiumintheEarth!flsmantle.TheamountofKpartitioningint
clinopyroxenedependsonthephaseassemblagepresent,th...
Lattice-dynamical evaluation of atomic displacement parameters of minerals and its implications: The example of diopside
Lattice-dynamical evaluation atomic displacement parameters minerals diopside
2012/4/6
ABorn-von Karman rigid-ion, lattice-dynamical model has been applied to diopside with the use of empirical potentials derived by fitting the vibrational frequencies of a group ofnesosilicates and oxid...
Structure refinement of a natural K-rich diopside: The effect of K on the average structure
Structure refinement natural K-rich diopside K average structure
2012/4/6
The crystal structure of the most K-rich natural pyroxene ever reported, a chromian diopside with1.5wt%K20,has been refined (diffractometer data, filtered MoKaradiation, by least-squares using XTAL to...
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...