Keshav, Shantanu, Corgne, Alexandre, Gudfinnsson, Gudmundur H., Bizimis, Michael, McDonough, William F., Fei, Yingwei (2005) Kimberlite petrogenesis: Insights from clinopyroxene-melt partitioning experiments at 6 GPa in the CaO-MgO-Al2O3-SiO2-CO2 system. Geochimica et Cosmochimica Acta, 69 (11) 2829-2845 doi:10.1016/j.gca.2005.01.012

See Also

These are possibly similar items as determined by title/reference text matching only.

	Corgne, Alexandre, Keshav, Shantanu, Wood, Bernard J., McDonough, William F., Fei, Yingwei (2008) Metal–silicate partitioning and constraints on core composition and oxygen fugacity during Earth accretion. Geochimica et Cosmochimica Acta, 72 (2) 574-589 doi:10.1016/j.gca.2007.10.006
	Corgne, Alexandre, Keshav, Shantanu, Fei, Yingwei, McDonough, William F. (2007) How much potassium is in the Earth's core? New insights from partitioning experiments. Earth and Planetary Science Letters, 256 (3) 567-576 doi:10.1016/j.epsl.2007.02.012
	Corgne, A., Keshav, S., Fei, Y., McDonough, W.F. (2006) How much potassium is in the Earth’s core? New insights from partitioning experiments. Geochimica et Cosmochimica Acta, 70 (18) doi:10.1016/j.gca.2006.06.140
	Keshav, Shantanu, Gudfinnsson, Gudmundur H (2021) A Reappraisal of Peridotite Solidus Phase Equilibria from 6 to 14 GPa in the System CaO–MgO–Al2O3–SiO2. Journal of Petrology, 62 (6) doi:10.1093/petrology/egab009
	Corgne, Alexandre, Armstrong, Lora S., Keshav, Shantanu, Fei, Yingwei, McDonough, William F., Minarik, William G., Moreno, Karen (2012) Erratum to: “Trace element partitioning between majoritic garnet and silicate melt at 10–17 GPa: Implications for deep mantle processes” [Lithos 148 (2012) 128–141]. Lithos, 154. 406 doi:10.1016/j.lithos.2012.07.005
	Corgne, Alexandre, Armstrong, Lora S., Keshav, Shantanu, Fei, Yingwei, McDonough, William F., Minarik, William G., Moreno, Karen (2012) Trace element partitioning between majoritic garnet and silicate melt at 10–17GPa: Implications for deep mantle processes. Lithos, 148. 128-141 doi:10.1016/j.lithos.2012.06.013
	Keshav, Shantanu, Corgne, Alexandre, Gudfinnsson, Gudmundur H., Fei, Yingwei (2020) Major and trace element partitioning between majoritic garnet and carbon dioxide-rich liquid in model carbonated peridotite at 10 GPa and interpretations of the element chemistry of majoritic garnet inclusions in diamonds from the subcontinental mantle of Brazil and Guinea. Lithos, 362. 105486 doi:10.1016/j.lithos.2020.105486
	Keshav, Shantanu, Gudfinnsson, Gudmundur H. (2010) Experimentally dictated stability of carbonated oceanic crust to moderately great depths in the Earth: Results from the solidus determination in the system CaO-MgO-Al2O3-SiO2-CO2. Journal of Geophysical Research, 115. doi:10.1029/2009jb006457
	Keshav, Shantanu, Gudfinnsson, Gudmundur H. (2013) Silicate liquid-carbonatite liquid transition along the melting curve of model, vapor-saturated peridotite in the system CaO-MgO-Al2O3-SiO2-CO2from 1.1 to 2 GPa. Journal of Geophysical Research: Solid Earth, 118 (7) 3341-3353 doi:10.1002/jgrb.50249
	Keshav, Shantanu, Hammouda, Tahar, Gudfinnsson, Gudmundur H (2022) Melting Phase Equilibria from 4 to 7 GPa in the System CaO-MgO-Al2O3-SiO2-CO2, the Persistence of the “Ledge” in Carbonated Basalt with Excess Silica, and the Most Likely Limits on the Depths of Termination of Carbon Cycle at Subduction Zones. Journal of Petrology, 63 (8) doi:10.1093/petrology/egac069
	Keshav, Shantanu, Bizimis, Michael, Gudfinnsson, Gudmundur H., Sen, Gautam, Fei, Yingwei (2006) Response to the comment by M. Lustrino on “High-pressure melting experiments on garnet clinopyroxenite and the alkalic–tholeiitic transition in ocean-island basalts” by Keshav et al. [Earth Planet. Sci. Lett. 223, 365–379 (2004)]. Earth and Planetary Science Letters, 241 (3) 997-999 doi:10.1016/j.epsl.2005.10.023