Boninitic metavolcanic rocks and island arc tholeiites from the Older Metamorphic Group (OMG) of Singhbhum Craton, eastern India: Geochemical evidence for Archean subduction processes
First report of boninite-low Ti arc basalt from Singhbhum Craton.
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Metasomatism of depleted mantle wedge by slab-dehydrated fluids during subduction initiation.
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Magma generation by flux-induced wedge melting in spinel peridotite domain of intraoceanic arc.
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Modern-style subduction processes during Paleo-Mesoarchean.
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