Systematics of detrital zircon U-Pb ages from Cambrian-Lower Devonian rocks of northern Morocco with implications for the northern Gondwanan passive margin

The systematic acquisition of U-Pb geochronological data from detrital zircon grains has become an essential tool in tectonic studies focused on reconstructing the pre-Variscan geography of the northern Gondwanan passive margin. New detrital zircon ages for 16 samples from the Cambrian-Lower Devonian succession of the Moroccan Mesetas (northern Morocco) are reported here. The results, combined with previously published data, reassert the strong West African Craton affinity of the Paleozoic sedimentary rocks, characterized by dominant Cadomian/Pan-African (c. 850-540 Ma) and Eburnean (c. 2.2-1.9 Ga) detrital zircon populations and a minor Leonian/Liberian (c. 2.5 Ga) population. Primary sources of these zircon grains are well established as the West African Craton located just to the south, but also in the Precambrian basement that locally crops out in the Moroccan Mesetas themselves. During the Cambrian-Early Ordovician, erosion preferentially dismantled Cadomian (c. 590-540 Ma) arc-derived rocks of the Gondwanan continental margin, while later, the slightly older Pan-African (c. 650-600 Ma) basement became the main sediment source. In the studied samples, irregularly present minor detrital zircon populations suggest additional sediment provenance from secondary sources such as: (i) remote northeastern African cratons (e.g., Saharan Metacraton and/or Arabian-Nubian Shield) that likely could have provided the c. 1.1-0.9 Ga and, possibly, the c. 1.9-1.7 Ga zircon grains, and (ii) rift-related Cambrian-Early Ordovician volcanic centers in the Moroccan Mesetas that supplied heterogeneously distributed - although locally dominant in small areas - sedimentary detritus before rift abortion and burial underneath the overlying passive margin sedimentary succession.

Automated summary

The detrital zircon ages from the Cambrian-Lower Devonian succession in the Moroccan Mesetas reveal a strong West African Craton affinity, with sources primarily from the West African Craton and locally from Precambrian basement rocks. Minor detrital zircon populations suggest additional sediment provenance from remote northeastern African cratons and rift-related volcanic centers in the Moroccan Mesetas during the Cambrian-Early Ordovician.