Systematic study of liquidas phase relations in olivine melilitite +H2O +CO2 at high pressures and petrogenesis of an olivine melilitite magma

Contributions to Mineralogy and Petrology

Volumn 61, Issue 2, 1977, Pages 141-162

  Brey, G ^a   Green, D H ^a  

^a AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0000961426     PISSN: 00107999     EISSN: 14320967     Source Type: Journal    
DOI: 10.1007/BF00374364     Document Type: Article

References (17)

1. Techniques for the control of water fugacity and oxygen fugacity for experimentation in solid-media high-pressure apparatus
2. CO2 solubility and solubility mechanisms in silicate melts at high pressures
3. The role of CO2 in the genesis of olivine melilitite
4. Solubility of CO2 in olivine melilitite at high pressures and role of CO2 in the earth's upper mantle
5. Role of CO2 in the melting processes in the mantle
6. Peridotite-carbonate relations in the system CaO-MgO-SiO2-CO2
7. The role of CO2 in the genesis of olivine melilitite: discussion
8. Orthopyroxene in the lunar interior and constraints on early lunar differentiation
9. Quantitative electron microprobe analysis using a lithium drifted silicon detector
10. Quantitative electron microprobe analysis of silicates using energy-dispersive X-ray spectrometry
11. Determination of the p, T paths of natural eclogites during metamorphism — record of subduction. A correction to a paper by Råheim and Green (1975)
12. The effect of reduced H2O fugacity on the buffering of oxygen fugacity in hydrothermal experiments
13. Carbonation and melting reactions in the system CaO-MgO-SiO2-CO2 at mantle pressures with geophysical and petrological applications