Abstract
Key Points The main Mesorif gabbros emplaced in a Liassic oceanic domain and do not belong to the Central Atlantic Magmatic Province (CAMP) CAMP dolerites may occur separately next to the oceanic gabbros in the structurally complex Mesorif zone The prerift/synrift cover of the distal margin could have emplaced by gravity sliding onto the Mesorif oceanic crust
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