Geochemical variations during Kilauea's Pu'u 'O'o Eruption reveal a fine-scale mixture of mantle heterogeneities within the Hawaiian Plume
Long-term geochemical monitoring of lavas from the continuing 25-year-old Pu'u 'Ōō eruption allows us to probe the crustal and mantle magmatic processes beneath Kīlauea volcano in unparalleled detail. Here we present new Pb, Sr, and Nd isotope ratios,
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|Source:||Journal of Petrology|
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