The transition between spinel lherzolite and garnet lherzolite, and its use as a Geobarometer

Contributions to Mineralogy and Petrology

Volumn 77, Issue 2, 1981, Pages 185-194

  O'Neill, Hugh St C ^a  

^a AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0019716158     PISSN: 00107999     EISSN: 14320967     Source Type: Journal    
DOI: 10.1007/BF00636522     Document Type: Article

References (45)

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3. Homogeneity of minerals in mantle rocks from Lesotho
4. Equilibrium cation distribution in NiAl2O4, CuAl2O4 and ZnAl2O4 spinels
5. Thermodynamic properties of almandine-grossular garnet solid solutions
6. Mg-Fe exchange equilibria among Al-Cr spinel, olivine, orthopyroxene and cordierite
7. Cell dimensions and X-ray determinative curve for synthetic Mg-Fe olivines
8. Hydrothermal synthesis and determination of equilibrium between minerals in the subliquidus region
9. Ordnung/Unordnung und Ultrarotabsorption. III. Die Systeme MgAl2O4-Al2O3 und MgAl2O4-LiAl5O8
10. The preparation of silicate compositions by a gelling method
11. Pyroxene geothermometry and geobarometry: experimental and thermodynamic evaluation of some subsolidus phase relations involving pyroxenes in the system CaO-MgO-Al2O3-SiO2
12. Chromian spinel as a petrogenetic indicator. I. Theory
13. Chromian spinel as a petrogenetic indicator. II. Petrologic applications
14. Experimental determination of the spinel peridotite to garnet peridotite inversion at 900° C and 1,000° C in the system CaO-MgO-Al2O3-SiO2, and at 900° C with natural garnet and olivine
15. Effect of pressure on garnetpyroxene equilibrium in the system MgSiO3-CaSiO3-Al2O3
16. Anorthite-forsterite and anorthite-enstatite reactions and their bearing on the basalt-eclogite transformation
17. Experimental studies on the system Fe-MgO-SiO2-O2, and their bearing on the petrology of chondritic meteorites
18. Stability fields of spinel and garnet peridotites in the synthetic system MgO-CaO-A12O3-SiO2
19. The effect of CaO, Cr2O3, Fe2O3 and Al2O3 on the stability of spinel and garnet peridotites
20. Iron II-magnesium exchange equilibrium between olivine and calcium-free pyroxene over a temperature range 800° C to 1,300° C
21. Unit cell dimensions of some synthetic orthopyroxene group solid solutions
22. Partitioning of Fe++ and Mg++ between coexisting synthetic olivine and orthopyroxene
23. Laboratory duplication of phase equilibria observed in natural garnet lherzolites
24. The thermodynamics of cation distribution in simple spinels
25. Pressure dependence of the enstatite limb of the enstatite-diopside solvus
26. Thermochemistry of high pressure garnets and clinopyroxenes in the system CaO-MgO-Al2O3-SiO2
27. The solubility of Al2O in orthopyroxene in spinel and plagioclase peridodites and spinel pyroxenite
28. Garnet-peridotite stability in crust and mantle
29. An experimental study of Fe-Mg partitioning between garnet and olivine and its calibration as a geothermometer
30. A model for the upper mantle
31. A reevaluation of the olivine-spinel geothermometer
32. Röntgenographische Untersuchung der Kationenverteilung in Spinellphasen
33. Experimental determination of univariant equilibria using divariant solid-solution assemblages
34. A direct determination of cation disorder in MgAl2O4 spinel by ESR
35. Thermodynamic properties of simple solutions
36. Synthesis and unit cell parameters of Ca-Mg-Fe pyroxenes
37. Solids solution and chromium oxide loss in part of the system MgO-Al2O3-Cr2O3-SiO2
38. Pyroxene thermometry in simple and complex systems
39. The solubility of alumina in orthopyroxene coexisting with garnet
40. The thermodynamic properties of reciprocal solid solutions