Eutectic between wollastonite II and calcite contrasted with thermal barrier in MgO-SiO2-CO2 at 30 kilobars, with applications to kimberlite-carbonatite petrogenesis
- 1 December 1974
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 24 (2) , 305-310
- https://doi.org/10.1016/0012-821x(74)90109-5
Abstract
No abstract availableKeywords
This publication has 12 references indexed in Scilit:
- The system CaOSiO2CO2H2O. II—The petrogenetic modelPublished by Elsevier ,2003
- Melting relationships in CaO-CO2 and MgO-CO2 to 36 kilobars with comments on CO2 in the mantleEarth and Planetary Science Letters, 1973
- Phase relationships of phlogopite in the system K 2 O-MgO-CaO-Al 2 O 3 -SiO 2 -H 2 O to 35 kilobars; a better model for micas in the interior of the EarthAmerican Journal of Science, 1973
- Melting curve of diopside to 50 kilobarsJournal of Geophysical Research, 1969
- The system CaO-SiO2-CO2-H2O—III. Second critical end-point on the melting curveGeochimica et Cosmochimica Acta, 1969
- Liquid immiscibility in the system Na 2 O-Al 2 O 3 -SiO 2 -CO 2 at pressures to 1 kilobarAmerican Journal of Science, 1966
- Melting relationships in the system CaO-MgO-SiO2-H2O at 1 kilobar pressureGeochimica et Cosmochimica Acta, 1966
- The system CaO-SiO2-CO2-H2O: 1. Melting relationships with excess vapor at 1 kilobar pressureGeochimica et Cosmochimica Acta, 1965
- Effects of pressure on the melting and polymorphism of enstatite, MgSiO3Journal of Geophysical Research, 1964
- Effect of pressure on the melting of diopside, CaMgSi2O6, and albite, NaAlSi3O8, in the range up to 50 kilobarsJournal of Geophysical Research, 1963