[PDF][PDF] Neotectonics of mainland Portugal: state of the art and future perspectives

J Cabral - Journal of Iberian Geology, 2012 - pdfs.semanticscholar.org
This paper presents a synthesis of the neotectonic studies performed in mainland Portugal
that address the “recent”(post Piacenzian,~ 3 Ma) tectonic evolution of the Portuguese …

Active faults in Iberia

C Sanz de Galdeano, JM Azañón, J Cabral… - The geology of Iberia: A …, 2019 - Springer
The distribution of active faults in the Iberian Peninsula is not homogeneous, being mainly
present, but not only, in areas affected by the Alpine Orogeny. They are located in several …

Building typologies identification to support risk mitigation at the urban scale–Case study of the old city centre of Seixal, Portugal

C Santos, TM Ferreira, R Vicente… - Journal of Cultural …, 2013 - Elsevier
The old urban centres are marks of an historical and architectural heritage that should be
protected and safeguarded. For such, it is fundamental to have a complete understanding of …

Simulations of strong ground motion in SW Iberia for the 1969 February 28 (Ms = 8.0) and the 1755 November 1 (M∼ 8.5) earthquakes - II. Strong ground motion …

R Grandin, JF Borges, M Bezzeghoud… - Geophysical Journal …, 2007 - academic.oup.com
This is the second paper of a series of two concerning strong ground motion in SW Iberia
due to earthquakes originating from the adjacent Atlantic area. The aim of this paper is to …

Seismic hazard impact of the Lower Tagus Valley fault zone (SW Iberia)

SP Vilanova, JFBD Fonseca - Journal of Seismology, 2004 - Springer
The seismic hazard of SW Iberia is composed of two contributions: offshore, large to very
large events on the plate boundary between Africa and Eurasia such as the Lisbon …

The 1531 Lisbon earthquake: A tsunami in the Tagus Estuary?

MA Baptista, JM Miranda… - Bulletin of the …, 2014 - pubs.geoscienceworld.org
Abstract On 26 January 1531, a strong‐magnitude earthquake heavily impacted Lisbon
downtown. Immediately after the earthquake, the eyewitnesses reported large waves in the …

As escadarias de terraços do Ródão à Chamusca (Baixo Tejo)–caracterização e interpretação de dados sedimentares, tectónicos, climáticos e do Paleolítico

PP Cunha, AA Martins, MP Gouveia - Estudos do Quaternário/Quaternary …, 2016 - apeq.pt
As unidades estratigráficas que resultaram da evolução do rio Tejo em Portugal, aqui
analisadas em pormenor entre Vila Velha de Ródão e Chamusca, possuem distintas …

Ground motion scenarios consistent with probabilistic seismic hazard disaggregation analysis. Application to Mainland Portugal

ML Sousa, A Campos Costa - Bulletin of Earthquake Engineering, 2009 - Springer
Probabilistic seismic hazard for Mainland Portugal was re-evaluated in order to perform its
disaggregation. Seismic hazard was disaggregated considering different spaces of random …

Evidence for coupled reverse and normal active faulting in W Iberia: The Vidigueira–Moura and Alqueva faults (SE Portugal)

AB da Silveira, J Cabral, H Perea, A Ribeiro - Tectonophysics, 2009 - Elsevier
The Vidigueira–Moura fault (VMF) is a 65 km long, E–W trending, N dipping reverse left-
lateral late Variscan structure located in SE Portugal (W Iberia), which has been reactivated …

Ground motion simulations of the SW Iberia margin: rupture directivity and earth structure effects

M Bezzeghoud, JF Borges, B Caldeira - Natural hazards, 2013 - Springer
In this study, we focus on the region between Gorringe Bank and the Horseshoe Fault
located in the SW Iberia margin, which is believed to be the site of the great 1755 …