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. - Archive ouverte HAL Accéder directement au contenu
Article Dans Une Revue Tectonics Année : 2020

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.

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Résumé

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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Dates et versions

hal-03736336 , version 1 (22-07-2022)

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A. Michard, Omar Saddiqi, A. Chalouan, M.C. Chabou, Philippe Lach, et al.. 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.. Tectonics, 2020, 39 (4), ⟨10.1029/2019tc006004⟩. ⟨hal-03736336⟩
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