Structural evidence of recent uplift at a small coastal area (S. Paio , Vila do Conde, NW Portugal)
Variscan granite and undeformed pegmatite veins intrude a metamorphic complex probably derived from a Precambrian-Lower Proterozoic crustal terrane (ZOM) accreted to the east to the core of the variscan orogen (ZCI) along a large deep crustal suture zone (ZCPT) that is recognized as a major neotecto...
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| Formato: | book |
| Idioma: | eng |
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2012
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| Texto completo: | https://hdl.handle.net/10216/73762 |
| País: | Portugal |
| Oai: | oai:repositorio-aberto.up.pt:10216/73762 |