The Alpine Orogeny in the West and Southwest Iberia Margins.

The Alpine orogeny is well recorded onshore and offshore by tectonic inversion of the Mesozoic rift basins. Large scale linear seamounts (more than 250 km long and with up to 5 km of uplift) involving oceanic and continental lithosphere were carried on top of thrusts, such as the Gorringe seamount a...

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Detalhes bibliográficos
Autor principal: Terrinha, Pedro (author)
Outros Autores: Ramos, Adrià (author), Neres, Marta (author), Valadares, Vasco (author), Duarte, João (author), Martinez-Loriente, Sara (author), Silva, Sónia (author), Mata, João (author), Kullberg, José Carlos (author), Casas-Sainz, Antonio (author), Matias, Luis (author), Fernández, Óscar (author), Muñoz, Josep Anton (author), Ribeiro, Carlos (author), Font, Eric (author), Neves, Conceição (author), Roque, Cristina (author), Rosas, Filipe (author), Pinheiro, Luis (author), Bartolomé, Rafael (author), Sallarès, Valentí (author), Magalhães, Vítor (author), Medialdea, Teresa (author), Somoza, Luis (author), Gràcia, Eulàlia (author), Hensen, Christian (author), Gutscher, Marc-André (author), Ribeiro, António (author), Zitellini, Nevio (author)
Formato: bookPart
Idioma:por
Publicado em: 2019
Assuntos:
Alpine orogeny
Southwest Iberian Margin
Texto completo:http://hdl.handle.net/10174/25763
País:Portugal
Oai:oai:dspace.uevora.pt:10174/25763

Texto Completo

http://hdl.handle.net/10174/25763

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