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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Bibliographic Details
Main Author: Terrinha, Pedro (author)
Other Authors: 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)
Format: bookPart
Language:por
Published: 2019
Subjects:
Alpine orogeny
Southwest Iberian Margin
Online Access:http://hdl.handle.net/10174/25763
Country:Portugal
Oai:oai:dspace.uevora.pt:10174/25763

Internet

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

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