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- W1964260725 abstract "Since the isotopic heterogeneity of ocean island basalts (OIB) is of variable character and requires billions of years to evolve, we propose to explain the observed heterogeneity by mixing between delaminated continental lithosphere, a continental crustal component, depleted mantle and pristine mantle. Such mixing occurs in a boundary layer located at the bottom of the upper mantle from which ascending blobs rise." @default.
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- W1964260725 date "1985-04-01" @default.
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- W1964260725 title "Geodynamic mixing in the mesosphere boundary layer and the origin of oceanic islands" @default.
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- W1964260725 doi "https://doi.org/10.1029/gl012i004p00207" @default.
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