Stability of phase A in antigorite (serpentine) composition determined by in situ X-ray pressure observations

Physics of the Earth and Planetary Interiors

Volumn 151, Issue 3-4, 2005, Pages 276-289

  Komabayashi, Tetsuya ^a   Hirose, Kei ^a   Funakoshi, Ken Ichi ^b   Takafuji, Naoto ^a  

^a TOKYO INSTITUTE OF TECHNOLOGY   (Japan)

^b JAPAN SYNCHROTRON RADIATION RESEARCH INSTITUTE   (Japan)

Author keywords

Double seismic zone; High pressure; Hydrous phase; In situ X ray diffraction; Subduction

Indexed keywords

CHLORITE MINERALS; DECOMPOSITION; DEHYDRATION; REACTION KINETICS; SEISMOLOGY; SERPENTINE; SODIUM CHLORIDE; SYNCHROTRONS; X RAY DIFFRACTION ANALYSIS;

ANTIGORITE COMPOSITIONS; LOW-PRESSURE STABILITY; MG-END-MEMBER ANTIGORITE; MULTI-ANVIL APPARATUS;

TECTONICS;

HIGH PRESSURE; PHASE TRANSITION; SERPENTINITE; SUBDUCTION ZONE; WATER CONTENT;

EID: 21844432394     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pepi.2005.04.002     Document Type: Article

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