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The Tethys Ocean was formed during the Late Paleozoic–Triassic era between the supercontinents Gondwana and Laurasia, characterized by diverse marine sediments and complex paleogeographic structures. Its growth was linked to the divergence of these plates, while its closure began in the Late Jurassic–Early Cretaceous due to continental convergence. The paleogeographic organization of Tethys was not simple like the Atlantic Ocean, but rather complex, involving multiple sedimentary facies and tectonic interac
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