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      Melting of Peridotites through to Granites: A Simple Thermodynamic Model in the System KNCFMASHTOCr

      1 , 2 , 3
      Journal of Petrology
      Oxford University Press (OUP)

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          Melting of a dry peridotite KLB-1 up to 14 GPa: Implications on the Origin of peridotitic upper mantle

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            Partial melting of dry peridotites at high pressures: Determination of compositions of melts segregated from peridotite using aggregates of diamond

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              The compressibility of silicate liquids containing Fe2O3 and the effect of composition, temperature, oxygen fugacity and pressure on their redox states

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                Author and article information

                Contributors
                (View ORCID Profile)
                Journal
                Journal of Petrology
                Oxford University Press (OUP)
                0022-3530
                1460-2415
                May 2018
                May 01 2018
                May 16 2018
                May 2018
                May 01 2018
                May 16 2018
                : 59
                : 5
                : 881-900
                Affiliations
                [1 ]Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, UK
                [2 ]Institute of Geochemistry and Petrology, ETH Zurich, Clausiusstrasse 25, Zurich, Switzerland
                [3 ]School of Earth Sciences, University of Melbourne, Parkville, Victoria, Australia
                Article
                10.1093/petrology/egy048
                941f5522-c670-488a-ae0f-071e2ffb84bf
                © 2018

                http://creativecommons.org/licenses/by/4.0/

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