Major element variations in Hawaiian shield lavas: Source features and perspectives from global ocean island basalt (OIB) systematics

[1] Among volcanic hot spots globally, Hawaii has the highest magma flux, yet there is significant controversy surrounding the composition of the mantle sourcing Hawaiian lavas. In order to place constraints on the source lithologies of Hawaiian lavas, we explore relationships between major elements and radiogenic isotopes in tholeiitic, shield-building lavas. Olivine-fractionation corrected lava compositions reveal clear trends between radiogenic isotopes and major elements. Individual data points exhibit remarkable trends and there is no need to average the data by volcano. Data form arrays that are anchored by Koolau lava at one end (with high Sr/Sr, Os/Os, SiO2, and Na2O/TiO2, and low Nd/Nd, Pb/Pb, TiO2, CaO and CaO/Al2O3) and by Kea and Loihi lavas at the other (with low Sr/Sr, Os/Os, SiO2, and Na2O/TiO2, and high Nd/Nd, Pb/Pb, TiO2, CaO and CaO/Al2O3). FeOtotal, Al2O3 and Na2O concentrations do not correlate with radiogenic isotopes. The Hawaiian data set exhibits correlations that mirror the best correlations between major elements and radiogenic isotope in the global ocean island basalt (OIB) database. We suggest that the mechanism driving the correlations in Hawaii illustrates, in microcosm, a larger global process that generates major element variability in mantle plumes. Like the global arrays, the Hawaiian lavas with radiogenic Pb and SiO2-poor lavas are sourced by a SiO2-poor mafic component (pyroxenite) admixed with peridotite, while Hawaiian lavas with unradiogenic Pb and high SiO2 are sourced by a SiO2-rich mafic component (eclogite). The variable SiO2 in the mafic component may result from different degrees of SiO2-extraction from the slab during subduction.