Can the Iberian Finisterra Terrane extends until Central Europe Variscides?
| dc.contributor.author | Moreira, Noel | |
| dc.contributor.author | Dias, Rui | |
| dc.contributor.author | Ribeiro, António | |
| dc.contributor.author | Romão, José | |
| dc.contributor.author | Noronha, Fernando | |
| dc.contributor.author | Pedro, Jorge | |
| dc.date.accessioned | 2018-02-20T15:30:47Z | |
| dc.date.available | 2018-02-20T15:30:47Z | |
| dc.date.issued | 2017 | |
| dc.description.abstract | The Finisterra Terrane is located in the western sector of the Iberian Variscides and its eastern boundary is a N-S to NNW-SSE lithospheric structure, the Porto-Tomar-Ferreira do Alentejo Shear Zone (PTFSZ). The PTFSZ makes the contact between the Finisterra Terrane and two distinct paleogeographic zones of the Iberian Terrane: Central Iberian and Ossa-Morena Zones. | por |
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| dc.identifier.citation | Moreira et al (2017) - Can the Iberian Finisterra Terrane extends until Central Europe Variscides?. Abstract book, pp.59,First International ASRO Geological Congress, El Jadida (Morocco). | por |
| dc.identifier.scientificarea | 249 | por |
| dc.identifier.uri | http://hdl.handle.net/10174/22381 | |
| dc.identifier.withinvitedoralpresentation | nao | por |
| dc.identifier.withoralpresentation | sim | por |
| dc.identifier.withposter | nao | por |
| dc.language.iso | por | por |
| dc.publisher | International ASRO Geological Congress | por |
| dc.rights | openAccess | por |
| dc.subject | Iberian Finisterra Terrane | por |
| dc.subject | Ossa-Morena Zone | por |
| dc.subject | Porto-Tomar-Ferreira do Alentejo Shear Zone | por |
| dc.subject | Central Iberian Zone | por |
| dc.title | Can the Iberian Finisterra Terrane extends until Central Europe Variscides? | por |
| dc.type | lecture | por |