Early Eocene clinoenstatite boninite and boninite-series dikes of the ophiolite of New Caledonia; a witness of slab-derived enrichment of the mantle wedge in a nascent volcanic arc
CE-boninite and boninite-series felsic dikes of New Caledonia yield Early Eocene 40Ar/39Ar and U–Pb zircon ages respectively
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Geochemical modeling suggest source enrichment by subduction-derived fluids and MORB-like melt component
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CE-boninite magma may have been in equilibrium with enstatite-bearing gabbro cumulates of the Peridotite Nappe
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