Phase boundary between perovskite and post-perovskite structures in MnGeO3 determined by in situ X-ray diffraction measurements using sintered diamond anvils

American Mineralogist

Volumn 96, Issue 1, 2011, Pages 89-92

  Yamazaki, Daisuke ^a   Ito, Eiji ^a   Katsura, Tomoo ^a   Yoshino, Takashi ^a   Zhai, Shuangmeng ^b   Fukui, Hiroshi ^c   Shatskiy, Anton ^d   Guo, Xinzhuan ^a   Shan, Shuangming ^a   Okuchi, Takuo ^a   Tange, Yoshinori ^e   Higo, Yuji ^f   Funakoshi, Ken Ichi ^f  

^a OKAYAMA UNIVERSITY   (Japan)

^b PEKING UNIVERSITY   (China)

^c UNIVERSITY OF HYOGO   (Japan)

^d TOHOKU UNIVERSITY   (Japan)

^e EHIME UNIVERSITY   (Japan)

^f JAPAN SYNCHROTRON RADIATION RESEARCH INSTITUTE   (Japan)

Author keywords

High pressure; In situ X ray observation; Phase boundary; Post perovskite

Indexed keywords

GERMANIUM COMPOUNDS; HIGH PRESSURE ENGINEERING; MAGNESIUM COMPOUNDS; MANGANESE COMPOUNDS; PHASE BOUNDARIES; SILICON COMPOUNDS; SINTERING; SYNCHROTRON RADIATION; X RAY DIFFRACTION;

CLAPEYRON SLOPE; HIGH PRESSURE; HIGH PRESSURE APPARATUS; IN-SITU X-RAY DIFFRACTION; POST PEROVSKITE; POST-PEROVSKITE STRUCTURE; SINTERED DIAMOND; SITU X RAY OBSERVATIONS;

PEROVSKITE;

DIAMOND ANVIL CELL; EXPERIMENTAL MINERALOGY; HIGH PRESSURE; HIGH TEMPERATURE; PEROVSKITE; PHASE EQUILIBRIUM; X-RAY DIFFRACTION;

EID: 79251543325     PISSN: 0003004X     EISSN: 19453027     Source Type: Journal    
DOI: 10.2138/am.2011.3499     Document Type: Article

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