The formation of Pangea
The making of Pangea is the result of large-scale amalgamation of continents and micro-continents, which started at the end of the Neoproterozoic with the formation of Gondwana. As pieces were added to Gondwana on its South-American, Antarctica and Australia side, ribbon-like micro-continents were d...
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Veröffentlicht in: | Tectonophysics 2013-05, Vol.593, p.1-19 |
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Format: | Artikel |
Sprache: | eng |
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