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There are two possible tectonic settings for the deep subduction of Indian Plate continental crust in the early Tertiary.
These extensional faults were reactivated as reverse faults during Neogene compression associated with subduction beneath the North Island.
subduction zone
Nevertheless, subduction of Africa beneath Iberia starting in the Late Eocene has been proposed.
The Spontang ophiolitc, for example, is associated with partial subduction of buoyant continental crust.
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