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Oceans isotope decoupling

Isotope decoupling between oceanic mantle and crust evidence for marble-cake or veined mantle 156... [Pg.805]

The loading matrix FA1/2 given by equation (4.4.26) can be found in Table 4.14. Lead isotopes have strong correlation coefficients on the first component. They are decoupled from Sr and Nd isotopes which strongly correlate and anticorrelate, respectively, with the second component. On a global scale, Pb isotopic variations in oceanic islands seem to be decoupled from Sr and Nd isotopic variations. [Pg.245]

Holmden C, Creaser RA, Muehlenbachs K, Leslie SA, Bergstrom SM (1998) Isotopic evidence for geochemical decoupling between ancient epeiric seas and bordering oceans Implications for secular curves. Geology 26 567-570... [Pg.601]

See other pages where Oceans isotope decoupling is mentioned: [Pg.817]    [Pg.858]    [Pg.859]    [Pg.115]    [Pg.156]    [Pg.157]    [Pg.230]    [Pg.280]    [Pg.858]    [Pg.938]    [Pg.989]    [Pg.1009]    [Pg.3403]    [Pg.3404]    [Pg.3404]    [Pg.4399]    [Pg.156]    [Pg.236]    [Pg.288]    [Pg.308]    [Pg.344]    [Pg.598]    [Pg.283]    [Pg.383]    [Pg.474]   
See also in sourсe #XX -- [ Pg.156 ]



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