GEOCHEMISTRY AND U-Pb ZIRCON AGE OF THE INTERNAL OSSA-MORENA ZONE OPHIOLITE SEQUENCES: A REMNANT OF RHEIC OCEAN IN SW IBERIA
The early Paleozoic geodynamic evolution in SW Iberia is believed to have been dominated by the opening of the Rheic Ocean. The Rheic Ocean is generally accepted to result from the drift of the peri-Gondwanan terranes such as Avalonia from the northern margin of Gondwana during the late Cambrian-ear...
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| Other Authors: | , , , |
| Format: | article |
| Language: | eng |
| Published: |
2011
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| Subjects: | |
| Online Access: | http://hdl.handle.net/10174/2553 |
| Country: | Portugal |
| Oai: | oai:dspace.uevora.pt:10174/2553 |