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Fig. 10

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Diagramme Pb-Pb des différents types de gisements et des feldspaths potassiques des districts d’Aouli (district de la Haute-Moulouya), de Touissit–Bou Beker–El Abed, et du Rif. Les champs A et B sont des champs de composition du granite d’Aouli à 230 et 180 Ma respectivement, avec μ = 9,74. Le champ des laves potassiques miocènes est d’après Duggen et al. (2005).

Pb-Pb diagram for the different types of ore deposits and K-feldspars of the Aouli (High-Moulouya), Touissit–Bou Beker–El Abed, and Rif districts. Fields A and B are compositional fields of Aouli granite at 230 and 180 Ma respectively, using μ = 9.74. Miocene potassic lava field is from Duggen et al. (2005).

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