Shantanu Keshav, Ph.D.
Affiliations: | 2004 | Florida International University, Miami, FL, United States |
Area:
GeochemistryGoogle:
"Shantanu Keshav"Mean distance: (not calculated yet)
Parents
Sign in to add mentor| Gautam Sen | grad student | 2004 | Florida International | |
| (An investigation into the Hawaiian mantle from a xenolithic perspective.) | ||||
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Publications
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| Keshav S, Corgne A, Gudfinnsson GH, et al. (2020) Major and trace element partitioning between majoritic garnet, clinopyroxene, 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 |
| Hammouda T, Keshav S. (2015) Melting in the mantle in the presence of carbon: Review of experiments and discussion on the origin of carbonatites Chemical Geology. 418: 171-188 |
| Keshav S, Gudfinnsson GH. (2014) Melting phase equilibria of model carbonated peridotite from 8 to 12 GPa in the system CaO-MgO-Al2O3-SiO2-CO2 and kimberlitic Liquids in the Earth's upper mantle American Mineralogist. 99: 1119-1126 |
| Novella D, Keshav S, Gudfinnsson GH, et al. (2014) Melting phase relations of model carbonated peridotite from 2 to 3 GPa in the system CaO-MgO-Al2O3-SiO2-CO2 and further indication of possible unmixing between carbonatite and silicate liquids Journal of Geophysical Research: Solid Earth. 119: 2780-2800 |
| Keshav S, Gudfinnsson GH. (2013) Silicate liquid-carbonatite liquid transition along the melting curve of model, vapor-saturated peridotite in the system CaO-MgO-Al<inf>2</inf>O <inf>3</inf>-SiO<inf>2</inf>-CO<inf>2</inf> from 1.1 to 2 GPa Journal of Geophysical Research: Solid Earth. 118: 3341-3353 |
| Corgne A, Armstrong LS, Keshav S, et al. (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 |
| Corgne A, Armstrong LS, Keshav S, et al. (2012) Trace element partitioning between majoritic garnet and silicate melt at 10-17GPa: Implications for deep mantle processes Lithos. 148: 128-141 |
| Keshav S, Gudfinnsson GH, Presnall DC. (2011) Melting phase relations of simplified carbonated peridotite at 12-26 gpa in the systems CaO-MgO-SiO |
| Keshav S, Gudfinnsson GH. (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-Al |
| Walter MJ, Bulanova GP, Armstrong LS, et al. (2008) Primary carbonatite melt from deeply subducted oceanic crust. Nature. 454: 622-5 |