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

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 ha...

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Bibliographic Details
Published in:Tectonics (Washington, D.C.) D.C.), 2020-04, Vol.39 (4), p.n/a
Main Authors: Michard, A., Saddiqi, O., Chalouan, A., Chabou, M.C., Lach, P., Rossi, P., Bertrand, H., Youbi, N.
Format: Article
Language:English
Subjects:
Earth Sciences
Mesozoic
Rifting
Sciences of the Universe
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Summary: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
ISSN:0278-7407
1944-9194
DOI:10.1029/2019TC006004