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.
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
Domaines
Sciences de la Terre
Fichier principal
Tectonics - 2020 - Michard - Comment on The Mesozoic Margin of the Maghrebian Tethys in the Rif Belt Morocco Evidence.pdf (3.79 Mo)
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