Abstract
In the Tizi n'Tichka area, the Late Ordovician sedimentation is characterized by two depositional sequences of glacio-eustatic origin: S1 and S2. Two other post-glacial sequences are proposed for the Lower Silurian deposits: at the Llandovery (S3) and at the Sheinwoodian (S4) ages. Their sea-level change curve is compared with curves from other continents.
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Schedule a callMore From: Comptes Rendus de l'Academie des Sciences Series IIA Earth and Planetary Science
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