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Nickel peridotite xenoliths

Figure 14 Covariation of V with AI2O3 in (a) abyssal peridotites, orogenic massifs, off-craton xenoliths, arc xenoliths, and (b) cratonic xenoliths (data sources in Table 6). Shown for illustrative purposes are residue trends for partial melting at 1.5 GPa as a functions of/o (expressed relative to the nickel-nickel oxide (NNO) buffer) calculated using methods described in Canil (2002). Figure 14 Covariation of V with AI2O3 in (a) abyssal peridotites, orogenic massifs, off-craton xenoliths, arc xenoliths, and (b) cratonic xenoliths (data sources in Table 6). Shown for illustrative purposes are residue trends for partial melting at 1.5 GPa as a functions of/o (expressed relative to the nickel-nickel oxide (NNO) buffer) calculated using methods described in Canil (2002).
See other pages where Nickel peridotite xenoliths is mentioned: [Pg.326]    [Pg.888]    [Pg.895]    [Pg.895]    [Pg.904]    [Pg.916]    [Pg.186]    [Pg.193]    [Pg.193]    [Pg.202]    [Pg.214]    [Pg.715]    [Pg.888]    [Pg.898]    [Pg.898]    [Pg.1077]    [Pg.1308]    [Pg.11]    [Pg.186]    [Pg.196]    [Pg.196]    [Pg.377]   
See also in sourсe #XX -- [ Pg.187 , Pg.195 , Pg.196 , Pg.197 ]



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