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. Article Swipe

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Geology Rift Mesozoic Paleontology Oceanic crust Margin (machine learning) Craton Passive margin Crust Polyphase system Geochemistry Tectonics Subduction Structural basin Engineering Machine learning Computer science Electronic engineering

André Michard , Omar Saddiqi , Ahmed Chaloüan , Moulley Charaf Chabou , Philippe Lach , Philippe Rossi , Hervé Bertrand , Nasrrddine Youbi ·

YOU? · · 2020 · Open Access · · DOI: https://doi.org/10.1029/2019tc006004 · OA: W3012377231

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

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. Article Swipe

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