Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
9529174 | Chemical Geology | 2005 | 11 Pages |
Abstract
We determined the structural changes in CaSiO3 and CaMgSi2O6 glasses recovered from high pressure and temperature conditions (up to 7.5 GPa and 500 °C) using X-ray diffraction, Raman, infrared and X-ray emission spectroscopy. Densities of the metasilicate glasses increase with applied pressure at high temperature; CaMgSi2O6 glass is more compressed than CaSiO3 glass when recovered from 7.5 GPa and 500 °C. We propose a mechanism for densification of these glasses, that is mainly due to the compaction in medium-range scale (i.e. decrease in cluster size of SiO4 anionic units with Ca, Mg polyhedra). Reduction of Si-O-Si bond angle is very small in the recovered CaSiO3 and CaMgSi2O6 glasses, as previously suggested.
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Authors
K. Shimoda, H. Miyamoto, M. Kikuchi, K. Kusaba, M. Okuno,