Petrogenesis of ultramafics in the Neoarchean Veligallu greenstone terrane, eastern Dharwar craton, India: Constraints from bulk-rock geochemistry and Lu-Hf isotopes
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文摘

We report Lu-Hf isotope systematics and infer the petrogenesis of ultramafic rocks.

The ultramafics are genetically related to the arc basalts.

Geochemical attributes indicate boninite-like affinity.

The basalt-ultramafic suite represents corresponding melt and derivative cumulate.

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