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      High-pressure partial melting of garnet pyroxenite: possible mafic lithologies in the source of ocean island basalts

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      Earth and Planetary Science Letters
      Elsevier BV

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          Mantle plumes from ancient oceanic crust

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            Dehydration Melting of Metabasalt at 8-32 kbar: Implications for Continental Growth and Crust-Mantle Recycling

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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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                Author and article information

                Journal
                Earth and Planetary Science Letters
                Earth and Planetary Science Letters
                Elsevier BV
                0012821X
                December 2003
                December 2003
                : 216
                : 4
                : 603-617
                Article
                10.1016/S0012-821X(03)00538-7
                42dc409a-74a8-405a-951a-9afb71ddc302
                © 2003

                http://www.elsevier.com/tdm/userlicense/1.0/

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