In the Ceuta area, located at the northernmost end of the Rifian Internal Zones, new outcrops of the Tertiary Formations covering Chomarid units, are studied. The new data obtained allow to characterize the Fnidek Formation (late Oligocene - Aquitanian p.p.) and to discover the Vinuela Formation of Burdigalian age. Furthermore, the discordance existing in between, is clearly evidenced here
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