Theoretical phase relations involving cordierite and garnet revisited: the influence of oxygen fugacity on the stability of sapphirine and spinel in the system Mg-Fe-Al-Si-O

Contributions to Mineralogy and Petrology

Volumn 92, Issue 3, 1986, Pages 362-367

  Hensen, B J ^a  

^a UNIVERSITY OF NEW SOUTH WALES   (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0022522599     PISSN: 00107999     EISSN: 14320967     Source Type: Journal    
DOI: 10.1007/BF00572165     Document Type: Article

References (16)

1. Stability of the assemblage orthopyroxene-sillimanite-quartz in the system MgO-FeO-Fe2O3-Al2O3-SiO2-H2O
2. Occurrence of sapphirine plus quartz at Peekskill, New York
3. Reaction textures and metamorphic evolution of sapphirine-bearing granulites from the Gruf Complex. Italian Central Alps
4. Osumilite-sapphirine-quartz granulites from Enderby Land Antarctica-Mineral assemblages and reactions
5. Buffering of pore fluids by metamorphic reactions
6. Osumilite in the sapphirine-quartz terrane of Enderby land, Antarctica: implications for osumilite petrogenesis in the granulite facies
7. Theoretical phase relations involving cordierite and garnet in the system MgO -FeO-Al2O3-SiO2
8. Experimental study of the stability of cordierite and garnet in pelitic compositions at high pressures and temperatures III. Synthesis of experimental data and geological applications
9. Experimental study of the stability of cordierite and garnet in pelitic compositions at high pressures and temperatures. I. Compositions with excess Alumino-Silicate
10. Selected phase relationships in the system Al-Mn-Fe-Si-O-H: A model for garnet equilibria
11. Granulite complex of the eastern part of the Stanovoy Fold Province and the Chogar facies of depth
12. Sapphirine bearing assemblages from Kiranur, Southern India: A study of chemographic relationships in the Na2O-FeO-MgO-Al2O3-SiO2-H2O system
13. An experimental determination of the high pressure stability limits of magnesian cordierite under wet and dry conditions
14. Spinel compositions as indicators of kinetically controlled local equilibrium in contact metamorphic emery
15. The spinel and quartz associations in high grade xenoliths from Tallante (S.E. Spain) and their potential use in geothermometry and barometry