Detrital zircon fingerprint of the Proto-Andes: Evidence for a Neoproterozoic active margin?
Neoproterozoic Palaeogeographic reconstructions of Rodinia conventionally place the western (Proto-Andean) margin of Amazonia against the eastern (Appalachian) margin of Laurentia. Separation and formation of the Iapetus Ocean is generally considered to have occurred later at ~550 Ma. We examine the...
| Main Authors: | , , , , , , |
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| Format: | Journal Article |
| Published: |
Elsevier BV
2008
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| Online Access: | http://hdl.handle.net/20.500.11937/5398 |