Transcurrent continental tectonics model
The Ossa-Morena Zone (SW Iberian Massif) was affected by continuous orogen-parallel transcurrent continental tectonics from the Neoproterozoic to the Carboniferous times, involving transtension (TT) and transpression (TP) processes that co-existed together, occurred separately in neighbouring region...
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| Formato: | article |
| Idioma: | eng |
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2011
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| Texto completo: | http://hdl.handle.net/10174/2970 |
| País: | Portugal |
| Oai: | oai:dspace.uevora.pt:10174/2970 |