Late Pleistocene and Holocene palaeogeography of the Lower Tagus Valley (Portugal): effects of relative sea level, valley morphology and sediment supply

GJ Vis, C Kasse, J Vandenberghe - Quaternary Science Reviews, 2008 - Elsevier
Because of the deep glacial incision, the Lower Tagus Valley hosts a sedimentary record
since∼ 20 000cal BP, making this a unique site along the European Atlantic margin with …

Lisbon 1755: a case of triggered onshore rupture?

SP Vilanova, CF Nunes… - Bulletin of the …, 2003 - pubs.geoscienceworld.org
It has been widely recognized, both in classical and in modern studies, that the Lisbon
earthquake of 1755 was a multiple event, composed of three shocks separated by a few …

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 …

Late Quaternary valley-fill succession of the Lower Tagus valley, Portugal

GJ Vis, C Kasse - Sedimentary Geology, 2009 - Elsevier
The Lower Tagus Valley in Portugal contains a well-developed valley-fill succession
covering the complete Late Pleistocene and Holocene periods. As large-scale stratigraphic …

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 …

Active surface faulting or landsliding in the Lower Tagus Valley (Portugal)? A solved controversy concerning the Vila Chã de Ourique site

JM Cabral, F Marques, P Figueiredo, L Matias - Journal of Seismology, 2011 - Springer
Abstract The Lower Tagus Valley has experienced significant (M 6–7) historical seismicity,
evidencing the presence of seismogenic faults. These are still deficiently known due to the …

[PDF][PDF] The 1531 Lisbon earthquake and tsunami

J Miranda, J Batlló, H Ferreira, LM Matias… - Paper 0685-15 World …, 2012 - iitk.ac.in
The 26 January 1531 earthquake heavily impacted Lisbon according to the coeval sources
and archaeological remnants. The earthquake, and in particular the claimed tsunami, were …

[引用][C] The 1531 Lisbon Earthquake: A Tsunami in the Tagus Estuary?

MABJM Miranda - Bulletin of the Seismological Society of America, 2014