Phase relations of CaAl4Si2O11 at high-pressure and high-temperature with implications for subducted continental crust into the deep mantle

Physics of the Earth and Planetary Interiors

Volumn 167, Issue 3-4, 2008, Pages 161-167

  Zhai, Shuangmeng ^a   Ito, Eiji ^a  

^a OKAYAMA UNIVERSITY   (Japan)

Author keywords

CaAl4Si2O11; Continental crust subduction; High pressure and temperature; Phase relation

Indexed keywords

GEOCHEMISTRY; HIGH PRESSURE EFFECTS; HIGH TEMPERATURE EFFECTS; PHASE INTERFACES; QUENCHING; STRUCTURAL GEOLOGY; TRACE ELEMENTS;

CONTINENTAL CRUST SUBDUCTION; PHASE RELATION;

GEOPHYSICS;

CONTINENTAL CRUST; CORUNDUM; GROSSULAR; HIGH PRESSURE; HIGH TEMPERATURE; KYANITE; MANTLE DISCONTINUITY; PHASE TRANSITION; PYROLITE; SLAB; SUBDUCTION; TRANSITION ZONE;

EID: 44349151742     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pepi.2008.03.004     Document Type: Article

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