U–Pb geochronology of Variscan granitoids from the Moroccan Meseta (Northwest Africa): Tectonic implications

Gondwana Research(2023)

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Abstract
•Two distinct Paleozoic magmatic pulses in the Meseta are distinguished.•The early Carboniferous one formed during the propagation of Paleotethys into the Gondwana margin.•The Late-Carboniferous – Early Permian pulse one formed during the closure of the Paleotehys.
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Key words
U–Pb zircon geochronology,Granitoids,Moroccan Meseta,Variscan belt
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