Articles | Volume 32, issue 2
Eur. J. Mineral., 32, 251–264, 2020
https://doi.org/10.5194/ejm-32-251-2020
Eur. J. Mineral., 32, 251–264, 2020
https://doi.org/10.5194/ejm-32-251-2020

Research article 23 Mar 2020

Research article | 23 Mar 2020

Melting relations of anhydrous olivine-free pyroxenite Px1 at 2 GPa

Giulio Borghini and Patrizia Fumagalli

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Cited articles

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Baker, M. B. and Stolper, E. M.: Determining the composition of high-pressure mantle melts using diamond aggregates, Geochim. Cosmochim. Acta, 58, 2811–2827, 1994. 
Basch, V., Rampone, E., Borghini, G., Ferrando, C., and Zanetti, A.: Origin of pyroxenites in the oceanic mantle and their implications on the reactive percolation of the depleted melts, Contrib. Mineral. Petrol., 174, 97, 2019. 
Bodinier, J.-L., Garrido, C. J., Chanefo, I., Bruguier, O., and Gervilla, F.: Origin of pyroxenite-peridotite veined mantle by refertilization reactions: Evidence from the Ronda peridotite (Southern Spain), J. Petrol., 49, 999–1025, 2008. 
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