2023
DOI: 10.1080/00206814.2023.2243498
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Tectonic controls on Late Cretaceous sedimentation on the southern Tethyan passive margin, Tunisia: new evidence of structural segmentation and early basin inversion

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Cited by 3 publications
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“…The NW-SE and NE-SW major faults and fractures are responsible for the metallurgic mechanism and the rise of deep water during water/rock contact, as well as having equally important roles in the rechargeability of surface-and shallow-water reservoirs by rainwater (Figure 2c). The geological, geomorphological and tectonic evolution of the rocks forming the major tectonic units of the study area can be traced back some 500 million years to when they were located on different continents (Gondwana and Laurasia) [19].…”
Section: Geological and Tectonic Settingmentioning
confidence: 99%
“…The NW-SE and NE-SW major faults and fractures are responsible for the metallurgic mechanism and the rise of deep water during water/rock contact, as well as having equally important roles in the rechargeability of surface-and shallow-water reservoirs by rainwater (Figure 2c). The geological, geomorphological and tectonic evolution of the rocks forming the major tectonic units of the study area can be traced back some 500 million years to when they were located on different continents (Gondwana and Laurasia) [19].…”
Section: Geological and Tectonic Settingmentioning
confidence: 99%