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

Verfasser: Norimasa, Nishiyama
Rapp, Robert
Irifune, Tetsuo
Sanehira, Takeshi
Yamazaki, D
Funakoshi, K
Dokumenttyp: Journal article
Verlag/Hrsg.: Springer
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-29096498
Datenquelle: BASE; Originalkatalog
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Link(s) : http://hdl.handle.net/1885/52438