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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

Norimasa, Nishiyama; Rapp, Robert; Irifune, Tetsuo; Sanehira, Takeshi; Yamazaki, D; Funakoshi, K

Description

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

CollectionsANU Research Publications
Date published: 2005
Type: Journal article
URI: http://hdl.handle.net/1885/52438
Source: Physics and Chemistry of Minerals
DOI: 10.1007/s00269-005-0037-y

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