West African provenance for Saxo-Thuringia (Bohemian Massif): Did Armorica ever leave pre-Pangean Gondwana? - U/Pb-SHRIMP zircon evidence and the Nd-isotopic record.
Neoproterozoic rocks in the Saxo-Thuringian part of Armorica formed in an active margin setting and were overprinted during Cadomian orogenic processes at the northern margin of Gondwana. The Early Palaeozoic overstep sequence in Saxo-Thuringia was deposited in a Cambro-Ordovician rift setting that...
| Main Authors: | , , , , , |
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| Format: | Journal Article |
| Published: |
Springer Verlag
2004
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/48177 |