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Evidence against an ancient non-chondritic mantle source for North Atlantic Igneous Province lavas
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文摘

Pervasive crustal contamination of North Atlantic Igneous Province melts

Tracking of primitive sources complicated by He isotope decoupling from lithophile isotopes

Crustal assimilation yields trends similar to those expected for an ancient non-chondritic source

Isotopic variability reflects recycled mantle heterogeneities and crustal contamination

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