Early Permian age of granite pebbles from an Eocene or Oligocene conglomerate of the Internal Rif belt (Alboran domain, Morocco): hypothesis on their origin

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Fig. 6

a. Multi-element patterns normalized to the primitive mantle (Wood et al., 1979) for the granites C2-4 (black square) and CG (white square). b. REE patterns normalized to chondrite (Sun and McDonough, 1989) for the granites C2-4 (black square) and CG (white square).

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