Sequence stratigraphic architecture and evolution history of the Late Cretaceous–Paleocene Assamoud carbonate platform, NE Sirte Basin, north-central Libya: Eustasy, tectonic, and inherited topography controls
Key Points
The sequence stratigraphic architecture reveals significant variations in the carbonate platform's evolution.
Key factors include eustasy and tectonic movements influencing depositional sequences across the region.
Observational analysis explores the Late Cretaceous to Paleocene period, focusing on geological formations and their changes.
Understanding these controls helps in reconstructing the paleoenvironments and geological history of NE Libya.
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Sequence stratigraphic architecture and evolution history of the Late Cretaceous–Paleocene Assamoud carbonate platform, NE Sirte Basin, north-central Libya: Eustasy, tectonic, and inherited topography controls | Synapse