Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6440703 | Lithos | 2015 | 13 Pages |
Abstract
The SiO2 content of clinopyroxene coexisting with garnet, coesite and kyanite is much higher than that of clinopyroxene coexisting with garnet and coesite without kyanite. Although the temperature dependence is unclear, the SiO2 solubility increases with pressure and Fe/(Fe+Mg). Clinopyroxene forms the solid solution series Jd-Es â¡0.5M0.5Al(Si,Ti)2O6 and Aug-Es, rather than Jd-Ts MAl2(Si,Ti)O6 and Es-Ts joins. Our experimental data suggest the probable existence of octahedral Si which may accompany the M2 vacancies in clinopyroxene.
Keywords
Related Topics
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Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Toshisuke Kawasaki, Yasuhito Osanai,