Melting experiment on a model chondritic mantle composition at 25 GPa
- 1 July 1987
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 14 (7), 733-736
- https://doi.org/10.1029/gl014i007p00733
Abstract
No abstract availableThis publication has 8 references indexed in Scilit:
- Majorite partition behavior and petrogenesis of the Earth's upper mantleGeophysical Research Letters, 1987
- Melting of a dry peridotite KLB‐1 up to 14 GPa: Implications on the Origin of peridotitic upper mantleJournal of Geophysical Research, 1986
- Melting of a model chondritic mantle to 20 GPaNature, 1986
- Incongruent melting of Mg2SiO4 at 20 GPaPhysics of the Earth and Planetary Interiors, 1985
- Stability Relations of Silicate Spinels, Ilmenites, and PerovskitesPublished by Springer Nature ,1982
- Thermal evolution of Earth and Moon growing by planetesimal impactsJournal of Geophysical Research, 1979
- Earth's melting due to the blanketing effect of the primordial dense atmosphereEarth and Planetary Science Letters, 1979
- PRESSURE CALIBRATION ABOVE 100 KBAR BASED ON THE NaCl INTERNAL STANDARDPublished by Elsevier ,1977