Please use this identifier to cite or link to this item: http://hdl.handle.net/10174/25763

Title: The Alpine Orogeny in the West and Southwest Iberia Margins.
Authors: Terrinha, Pedro
Ramos, Adrià
Neres, Marta
Valadares, Vasco
Duarte, João
Martinez-Loriente, Sara
Silva, Sónia
Mata, João
Kullberg, José Carlos
Casas-Sainz, Antonio
Matias, Luis
Fernández, Óscar
Muñoz, Josep Anton
Ribeiro, Carlos
Font, Eric
Neves, Conceição
Roque, Cristina
Rosas, Filipe
Pinheiro, Luis
Bartolomé, Rafael
Sallarès, Valentí
Magalhães, Vítor
Medialdea, Teresa
Somoza, Luis
Gràcia, Eulàlia
Hensen, Christian
Gutscher, Marc-André
Ribeiro, António
Zitellini, Nevio
Editors: Quesada, C.
Oliveira, J.
Keywords: Alpine orogeny
Southwest Iberian Margin
Issue Date: 2019
Publisher: Springer
Citation: Terrinha P. et al. (2019) The Alpine Orogeny in the West and Southwest Iberia Margins. In: Quesada C., Oliveira J. (eds) The Geology of Iberia: A Geodynamic Approach. Regional Geology Reviews. Springer, Cham
Abstract: 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 and the Estremadura Spur in the SouthWest and West Iberia Margin, respectively. The SouthWest Iberia Margin also recorded the westward migration of the Gibraltar Oceanic slab as the westwards propagation of the Neo-Tethys subduction. Rotation of the tectonic compression from NW-SE to WNW-ESE in Pliocene times caused the development of large scale dextral wrench faults as the present day Africa-Iberia plate boundary. Neotectonics of this plate boundary caused large to mega-scale destructive earthquakes and tsunamis.
URI: https://link.springer.com/chapter/10.1007%2F978-3-030-11295-0_11
http://hdl.handle.net/10174/25763
Type: bookPart
Appears in Collections:ICT - Publicações - Capítulos de Livros

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