Distribution of the Late Jurassic Dykes of the Central High Atlas and Tectonic Implications

Summary Inventory of dyke swarms in the Central High Atlas reveals at least 303 dykes, spanning 646 visible km in outcrop. Their predominantly unidirectional ENE-WSW strike may indicate a NNW-SSE extensional event from Mid-Jurassic to Early Cretaceous times, potentially linked to large intrusions in the Central High Atlas. These intrusions are thought to have occupied the crustal levels of the basin, as suggested by tomographic studies. The NNW-SSE direction of extension contradicts compressional tectonics and raises questions about the emplacement of intrusions along releasing stepovers and bends, as proposed in previous models. Therefore, an extensional event appears to be a more plausible explanation for the post-Middle Jurassic magmatism.

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Published
2025-01-01
DOI
https://doi.org/10.3997/2214-4609.2025639028
Primary Topic
Geological and Geophysical Studies Worldwide
Type
article
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article

Distribution of the Late Jurassic Dykes of the Central High Atlas and Tectonic Implications

Moulay Ahmed Boumehdi, Andrea Marzoli, Nasrrddine Youbi, Hassan Ibouh et al.
Geological and Geophysical Studies Worldwide
article

Distribution of the Late Jurassic Dykes of the Central High Atlas and Tectonic Implications

Moulay Ahmed Boumehdi, Andrea Marzoli, Nasrrddine Youbi, Hassan Ibouh, Fida Medina, Hervé Bertrand
article en

Abstract

Summary Inventory of dyke swarms in the Central High Atlas reveals at least 303 dykes, spanning 646 visible km in outcrop. Their predominantly unidirectional ENE-WSW strike may indicate a NNW-SSE extensional event from Mid-Jurassic to Early Cretaceous times, potentially linked to large intrusions in the Central High Atlas. These intrusions are thought to have occupied the crustal levels of the basin, as suggested by tomographic studies. The NNW-SSE direction of extension contradicts compressional tectonics and raises questions about the emplacement of intrusions along releasing stepovers and bends, as proposed in previous models. Therefore, an extensional event appears to be a more plausible explanation for the post-Middle Jurassic magmatism.

Université Claude Bernard Lyon 1 (FR), École Normale Supérieure de Lyon (FR), Cadi Ayyad University (MA), Centre National de la Recherche Scientifique (FR), University of Padua (IT), University of Lisbon (PT), National Research Tomsk State University (RU), Moroccan Foundation for Advanced Science, Innovation and Research (MA), Laboratoire de Géologie de Lyon : Terre, Planètes et Environnement (FR)
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Geological and Geophysical Studies Worldwide
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