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  • curprev 19:44, 28 March 2016Molyneux talk contribs 548 bytes +548 Paleogeographic maps of Libya. (A) Pan-African structures that formed during late Precambrian to Late Carboniferous tectonism. (B) Hercynian structural trends caused by the Late Carboniferous collision between Gondwana and Laurasia. Sources: Klitzsch (...