Fig. 2
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Paleogeographic map for the Lias epoch, modified in Frizon de Lamotte et al. (2008) after Jabour et al. (2003-2004). The most important modification from the original figure concerns the West Moroccan Arch, which is no longer regarded as a Liassic emergent land, but as a shallow platform eroded during the late Middle Jurassic-Early Cretaceous interval.
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