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The results of various recent geophysical studies suggest that the southern New Hebrides Basin and the western South Fiji Basin were once a single marginal basin. The basin originated above an ancient subduction of the Indian Plate under the Pacific Plate, active during Eocene-Oligocene. The ‘fossil’ subduction zone stretched along the western side of the Loyalty Rise and the Three Kings Rise both of which would have then belonged to the same volcanic arc.
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