Geology Of Tunisia
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Geology Of Tunisia
The geology of Tunisia is defined by the tectonics of North Africa, with large highlands like the Atlas Mountains as well as basins such as the Tunisian Trough. Geologists have identified rock units in the country as much as a quarter-billion years old, although most units date to the Mesozoic and Cenozoic, in the past 250 million years. Tunisia has a small but active mining industry and a significant oil and natural gas sector. Structural Geology & Tectonics The Tunisian Atlas mountains are a fold and thrust belt between the Rifo-Tellian chain, in the northwest (a part of the Alpine chain) and the Saharan platform in southern Tunisia. The Rifo-Tellian chain is separated from the Atlas Mountains in northern Tunisia by the Tunisian Trough. Sedimentary units in the Tunisian Atlas mountains are divided by three regional faults: the Kasserine Fault, Gafsa Fault and Kaala-Djerda-Sbiba Fault. Stratigraphy & Geologic History The oldest strata in Tunisia date to the Permian and ...
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Mesozoic
The Mesozoic Era ( ), also called the Age of Reptiles, the Age of Conifers, and colloquially as the Age of the Dinosaurs is the second-to-last era of Earth's geological history, lasting from about , comprising the Triassic, Jurassic and Cretaceous Period (geology), Periods. It is characterized by the dominance of archosaurian reptiles, like the dinosaurs; an abundance of conifers and ferns; a hot Greenhouse and icehouse earth, greenhouse climate; and the tectonic break-up of Pangaea. The Mesozoic is the middle of the three eras since Cambrian explosion, complex life evolved: the Paleozoic, the Mesozoic, and the Cenozoic. The era began in the wake of the Permian–Triassic extinction event, the largest well-documented mass extinction in Earth's history, and ended with the Cretaceous–Paleogene extinction event, another mass extinction whose victims included the non-avian dinosaurs, Pterosaur, pterosaurs, Mosasaur, mosasaurs, and Plesiosaur, plesiosaurs. The Mesozoic was a time of ...
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