Comment on “The Mesozoic Margin of the Maghrebian Tethys in the Rif Belt (Morocco): Evidence for Polyphase Rifting and Related Magmatic Activity” by Gimeno‐Vives et al.

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