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The Pan-African orogeny was a series of major Neoproterozoic orogenic events (mountain building) which related to the formation of the supercontinents Gondwana and Pannotia about 600 million years ago.[1] References 1. ^ "Glossary of Plate Tectonic and Paleogeographic Terms" (PDF). http://www.dinodata.net/Golonka/GLOSSARY.pdf. Retrieved 2006-04-09. (not available without registration (free)) Retrieved from "http://en.wikipedia.org/"
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