Internally consistent thermodynamic data set for dense hydrous magnesium silicates up to 35 GPa, 1600 °C: Implications for water circulation in the Earth's deep mantle

Physics of the Earth and Planetary Interiors

Volumn 156, Issue 1-2, 2006, Pages 89-107

  Komabayashi, Tetsuya ^a   Omori, Soichi ^a  

^a TOKYO INSTITUTE OF TECHNOLOGY   (Japan)

Author keywords

High pressure; Hydrous phase; Thermodynamic data; Water circulation

Indexed keywords

DEHYDRATION; GEOLOGY; HIGH PRESSURE EFFECTS; LINEAR PROGRAMMING; MAGNESIUM COMPOUNDS; SERPENTINE; SILICATE MINERALS; THERMODYNAMIC PROPERTIES; THERMODYNAMICS;

DENSE HYDROUS MAGNESIUM SILICATES; DRY MANTLE MINERALS; FLUID PHASE; FLUID-UNSATURATED HIGH-PRESSURE; PETROGENETIC GRID; POST-SERPENTINE PHASE; WATER-BEARING TRANSITION ZONE;

EARTH (PLANET);

HIGH PRESSURE; LINEAR PROGRAMING; MAGNESIUM; MANTLE STRUCTURE; PHASE EQUILIBRIUM; SILICATE; SLAB;

EID: 33646583824     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pepi.2006.02.002     Document Type: Article

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