Stability of hydrous magnesium silicates in the mantle transition zone

Physics of the Earth and Planetary Interiors

Volumn 66, Issue 3-4, 1991, Pages 307-312

  Kanzaki, Masami ^a  

^a UNIVERSITY OF ALBERTA   (Canada)

Author keywords

[No Author keywords available]

Indexed keywords

HYDROUS PHASE; MAGNESIUM SILICATE; MANTLE TRANSITION ZONE; PHASE RELATIONS; STABILITY FIELD;

EID: 0026003989     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/0031-9201(91)90085-V     Document Type: Article

References (17)

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5. Melting experiments on chondrodite at high pressures: stability of anhydrous phase B
6. Ultrahigh-pressure phase transformations and the constitution of the deep mantle
7. Stability of phase B, a hydrous magnesium silicate, to 2300°C at 20 GPa
8. Melting experiments of natural lherzolite at 20 GPa: formation of phase B coexisting with garnet
9. Phase transformations in serpentine at high pressures and temperatures and implications for subducting lithosphere
10. 2O in the phase behavior of the forsterite-enstatite system at high pressures and temperatures and implications for the Earth
11. Silicate and germanate garnets, ilmenites and perovskites: thermochemistry, lattice vibrations and spectroscopy
12. 2O
13. 2O
14. 2O
15. 2O at high pressures and temperatures—stability field for hydroxyl-chondrodite, hydroxyl-clinohumite and 10 Å-phase