Post-spinel transition in Mg2SiO4 determined by high P - T in situ X-ray diffractometry

Physics of the Earth and Planetary Interiors

Volumn 136, Issue 1-2, 2003, Pages 11-24

  Katsura, Tomoo ^a   Yamada, Hitoshi ^a   Shinmei, Toru ^a   Kubo, Atsushi ^a   Ono, Shigeaki ^a   Kanzaki, Masami ^a   Yoneda, Akira ^a   Walter, Michael J ^a   Ito, Eiji ^a   Urakawa, Satoru ^a   Funakoshi, Kenichi ^a,b   Utsumi, Wataru ^a,c  

^a OKAYAMA UNIVERSITY   (Japan)

^b JAPAN SYNCHROTRON RADIATION RESEARCH INSTITUTE   (Japan)

^c JAPAN ATOMIC ENERGY AGENCY   (Japan)

Author keywords

660 km discontinuity; High pressures and temperatures; In situ X ray diffractometry; Mantle; Mg2SiO4; Post spinel transition

Indexed keywords

MANTLE; P-T CONDITIONS; PHASE TRANSITION; SPINEL; TRANSITION ZONE; X-RAY DIFFRACTION;

EID: 0037531586     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0031-9201(03)00019-0     Document Type: Article

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