Stability and P-V-T equation of state of KAISi 3 O 8 -hollandite determined by in situ X-ray observations and implications for dynamics of subducted continental crust material
In situ X-ray diffraction measurements of KAlSi3O8 -hollandite (K-hollandite) were performed at pressures of 15-27 GPa and temperatures of 300-1,800 K using a Kawai-type apparatus. Unit-cell volumes obtained at various pressure and temperature conditions
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| Dokumenttyp: | Journal article |
| Verlag/Hrsg.: |
Springer
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| Schlagwörter: | Keywords: Equations of state / Phase transitions / Potassium compounds / Tectonics / Thermal expansion / Thermodynamic properties / X ray diffraction analysis / Continental crust / Hollandite / Phase boundary / Silicates / P-T conditions / phase transition / subduction zone / X- Continental crust / Equation of state / High pressure and temperature / K-hollandite |
| Sprache: | unknown |
| Permalink: | https://search.fid-benelux.de/Record/base-26734442 |
| Datenquelle: | BASE; Originalkatalog |
| Powered By: | BASE |
| Link(s) : | http://hdl.handle.net/1885/52438 |
