Abstract
The polyphase Mauritanide belt has been gradually developed from south to north during three major orogenic events, Panafrican, Taconian and Early Hercynian. The present aspect of the belt is due to superposition of Hercynian elements (internal nappes) on both Taconian and Panafrican elements (external nappes). These nappes cover the northern two-thirds of the belt and overthrust the West African shield and its Upper Proterozoic to Palaeozoic cover to the east. Taconian and Panafrican elements in parautochthonous, locally allochthonous position occupy the southern third of the belt. A discussion of the arguments for the present interpretation emphasizes the problems being solved.
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© 1983 D. Reidel Publishing Company, Dordrecht, Holland
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Lecorche, JP. (1983). Structure of the Mauritanides. In: Schenk, P.E., Haworth, R.T., Keppie, J.D., Trzcienski, W.E., Williams, P.F., Kelling, G. (eds) Regional Trends in the Geology of the Appalachian-Caledonian-Hercynian-Mauritanide Orogen. NATO ASI Series, vol 116. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-7239-1_33
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DOI: https://doi.org/10.1007/978-94-009-7239-1_33
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