Titlebook: Geology of North Africa and the Mediterranean: Sedimentary Basins and Georesources; Sami Khomsi,Francois Roure Book 2023 Springer Nature S

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Ordovician–Upper Silurian–Triassic Petroleum System Assessment in the Chotts Areasupplied Ordovician and Triassic clastic reservoirs in the area. However, various debates are still held regarding either the source rock distribution and thermal maturity but also the reservoirs viability and extension. Within this scope, this study focussed on the evaluation and the characterizati

anatomical

An Overview of the Eastern Atlas Fold and Thrust Belt and Its Foreland Basin Along the North–South Athe South Atlasic Front (SAF) and its relations with the Ktitir platform and Chorbane major structural anomaly. Different subsurface interpretations allow deciphering the major tectonic pulses in the Eastern Atlas and its foreland basin, from Jurassic–Early Cretaceous rifting to Upper Cretaceous–Lat

Frequency

Aquifer Structuring and Hydrogeological Investigation in North African Regions Using Geophysical Metydrogeological data. Gravity methods analysis, seismic reflection, wireline logging, and electrical resistivity tomography techniques are used to identify the lithological and geometrical knowledge of the Mio-Plio-Quaternary aquifer in the Kairouan plain. In the Kairouan region, the Mio-Plio-Quatern

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Eclampsia

The Tellian Units, the Sellaoua Window and the High Medjerda Foreland in the Souk Ahras Area, NE Alg (Ouled Driss Sector), and shallow marine nummulitid facies to the south (Boukebch and Dekma areas), both have been unconformably covered by the Miocene. The Tellian thrust sheets of the Souk Ahras region exhibit a duplex geometry in the northern sector and an imbricate fan of thrusts to the south.

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Facies Analyses and Basin Evolution of the Cretaceous-Tertiary Rift-Related Sedimentary Succession o settings under short-lived periods of sea level fluctuation and (3) an upper fluvio-lacustrine member which is completely similar in lithologic characters and depositional environments to the lower member. This indicates the second regime of block faulting and reactivation and deposition of alluvia

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