This question is for an updated paleogeographical reconstruction of the Atlas Gulf and assiociated landmasses in the Early Jurassic (Early Toarcian)
We know that this Paleozoic montane rangue was exposed on the EJ (Frizon de Lamotte et al., 2008), that was being pushed by two rift systems (the Tethyan Atlas rift in the north and the Atlantic rift in the west) and that there was an ongoing exhumation, that cutaround 7.5–10.5 km of crustal rocks by the end of the Middle Jurassic (Gouiza et al., 2017). As well there is evidence it was a source for siliclastic materials in the Early Jurassic Atlas Gulf (Krencker et al. 2020).
But, is there any suggested reconstrucion of it´s appperance? Or a suggestion of what it may have looked like?
-Frizon de Lamotte, D., Zizi, M., Missenard, Y., Hafid, M., Azzouzi, M. E., Maury, R. C., ... & Michard, A. (2008). The atlas system. Continental Evolution: The Geology of Morocco: Structure, Stratigraphy, and Tectonics of the Africa-Atlantic-Mediterranean Triple Junction, 133-202.
-Gouiza, M., Charton, R., Bertotti, G., Andriessen, P., & Storms, J. E. A. (2017). Post-Variscan evolution of the Anti-Atlas belt of Morocco constrained from low-temperature geochronology. International Journal of Earth Sciences, 106, 593-616.
-Krencker, F. N., Fantasia, A., Danisch, J., Martindale, R., Kabiri, L., El Ouali, M., & Bodin, S. (2020). Two-phased collapse of the shallow-water carbonate factory during the late Pliensbachian–Toarcian driven by changing climate and enhanced continental weathering in the Northwestern Gondwana Margin. Earth-Science Reviews, 208, 103254.