Melting experiments on anhydrous peridotite KLB‐1 from 5.0 to 22.5 GPa
- 10 September 1994
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 99 (B9), 17729-17742
- https://doi.org/10.1029/94jb01406
Abstract
No abstract availableKeywords
This publication has 39 references indexed in Scilit:
- Partitioning “equilibrium”, temperature gradients, and constraints on Earth differentiationEarth and Planetary Science Letters, 1989
- Crystal chemistry of phase B and an anhydrous analogue: implications for water storage in the upper mantleNature, 1989
- Mass balance and phase density constraints on early differentiation of chondritic mantleEarth and Planetary Science Letters, 1988
- Constraints on element partition coefficients between MgSiO3 perovskite and liquid determined by direct measurementsEarth and Planetary Science Letters, 1988
- Melting experiment on natural lherzolite at 20 GPa: Formation of phase B coexisting with garnetGeophysical Research Letters, 1986
- Garnet‐perovskite transformation in CaGeO3: In‐situ X‐ray measurements using synchrotron radiationGeophysical Research Letters, 1985
- Origin of mantle peridotite and komatiite by partial meltingGeophysical Research Letters, 1985
- Melting of peridotite to 14 GPa and the genesis of komatiiteNature, 1985
- Solidus and liquidus temperatures and mineralogies for anhydrous garnet-lherzolite to 15 GPaPhysics of the Earth and Planetary Interiors, 1983
- Formation and fractionation of basic magmas at high pressuresScottish Journal of Geology, 1967