Pan-African orogeny

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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 900 million years ago.[1]

[edit] References

  1. ^ Glossary of Plate Tectonic and Paleogeographic Terms (PDF). Retrieved on 2006-04-09.
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