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Palaeoenvironmental And Tectonic Significance Of Miocene Lacustrine And Palustrine Carbonates (Ait Kandoula Formation, Ouarzazat.pdf

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Summary

The Ouarzazate Basin in Morocco contains a sedimentary fill recording the interplay between tectonics, climate, and surface processes from the Eocene to Pleistocene. Analysis of the Middle to Late Miocene Aït Kandoula Formation reveals five sedimentary facies of lacustrine and palustrine limestones, with two facies associations related to water depth and sub-aerial exposure. Stable isotope analysis shows strong covariance in early carbonates, indicating a hydrologically closed basin, but late Tortonian to Messinian carbonates suggest an externally draining, balanced-fill lacustrine system, questioning the established view of tectonic stagnation in the High Atlas Mountains' development.

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The Ouarzazate Basin in Morocco contains a sedimentary fill recording the interplay between tectonics, climate, and surface processes from the Eocene to...

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