Evidence of Surface Rupture Associated With Historical Earthquakes in the Lower Tagus Valley, Portugal. Implications for Seismic Hazard in the Greater Lisbon Area

The Lower Tagus Valley Fault, Portugal, has long been associated with the damaging earthquakes that affected the Greater Lisbon Area in historical times. These include a poorly documented earthquake that occurred in 1344, the relatively well-documented 1531 earthquake, and the most recent M6.0 1909...

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Main Authors: Carolina Canora, Susana P. Vilanova, Yolanda De Pro-Diáz, Pedro Pina, Sandra Heleno
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-03-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2021.620778/full
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spelling doaj-0daff8590e8d4be4bed7a227913086d12021-03-03T05:28:03ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632021-03-01910.3389/feart.2021.620778620778Evidence of Surface Rupture Associated With Historical Earthquakes in the Lower Tagus Valley, Portugal. Implications for Seismic Hazard in the Greater Lisbon AreaCarolina Canora0Susana P. Vilanova1Yolanda De Pro-Diáz2Pedro Pina3Sandra Heleno4Departamento de Geología y Geoquímica, Facultad de Ciencias, Universidad Autónoma de Madrid, Madrid, SpainCentre for Natural Resources and the Environment (CERENA), Instituto Superior Técnico, Lisboa, PortugalDepartamento de Geodinámica, Estratigrafía y Paleontología, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, Madrid, SpainCentre for Natural Resources and the Environment (CERENA), Instituto Superior Técnico, Lisboa, PortugalCentre for Natural Resources and the Environment (CERENA), Instituto Superior Técnico, Lisboa, PortugalThe Lower Tagus Valley Fault, Portugal, has long been associated with the damaging earthquakes that affected the Greater Lisbon Area in historical times. These include a poorly documented earthquake that occurred in 1344, the relatively well-documented 1531 earthquake, and the most recent M6.0 1909 earthquake. In this work, we use a 0.5 m resolution LiDAR-based digital elevation model and a 0.5 cm resolution digital surface model based on UAV photogrammetry to accurately locate the fault scarps in the northernmost portion of the western fault strand and to select sites to perform paleoseimolological investigations. The paleoseismological and geochronological analysis performed in the Alviela trench site document the fault activity in the last 3000 years, including two earthquakes during historical times. We performed ground motion scenarios for 20 km, 40 km, and 60 km ruptures including the trench site. The ground motion fields obtained for the 40 km and 60 km ruptures are in agreement with most macroseismic intensity data available for the 1531 earthquake, implying a magnitude in the range M6.8–7.4. However, the degree of deformation preserved in the trench suggests a value closer to the lower magnitude bound. The intensity level observed in Lisbon in 1531 (IX) is lower than the modeled intensities for all considered scenarios and could be related to a particularly high level of vulnerability of the building stock.https://www.frontiersin.org/articles/10.3389/feart.2021.620778/fulllower Tagus valley fault zoneLisbon 1531 earthquakeactive faultingpaleoseismology trenchingground motion scenariosmacroseismic intensity
collection DOAJ
language English
format Article
sources DOAJ
author Carolina Canora
Susana P. Vilanova
Yolanda De Pro-Diáz
Pedro Pina
Sandra Heleno
spellingShingle Carolina Canora
Susana P. Vilanova
Yolanda De Pro-Diáz
Pedro Pina
Sandra Heleno
Evidence of Surface Rupture Associated With Historical Earthquakes in the Lower Tagus Valley, Portugal. Implications for Seismic Hazard in the Greater Lisbon Area
Frontiers in Earth Science
lower Tagus valley fault zone
Lisbon 1531 earthquake
active faulting
paleoseismology trenching
ground motion scenarios
macroseismic intensity
author_facet Carolina Canora
Susana P. Vilanova
Yolanda De Pro-Diáz
Pedro Pina
Sandra Heleno
author_sort Carolina Canora
title Evidence of Surface Rupture Associated With Historical Earthquakes in the Lower Tagus Valley, Portugal. Implications for Seismic Hazard in the Greater Lisbon Area
title_short Evidence of Surface Rupture Associated With Historical Earthquakes in the Lower Tagus Valley, Portugal. Implications for Seismic Hazard in the Greater Lisbon Area
title_full Evidence of Surface Rupture Associated With Historical Earthquakes in the Lower Tagus Valley, Portugal. Implications for Seismic Hazard in the Greater Lisbon Area
title_fullStr Evidence of Surface Rupture Associated With Historical Earthquakes in the Lower Tagus Valley, Portugal. Implications for Seismic Hazard in the Greater Lisbon Area
title_full_unstemmed Evidence of Surface Rupture Associated With Historical Earthquakes in the Lower Tagus Valley, Portugal. Implications for Seismic Hazard in the Greater Lisbon Area
title_sort evidence of surface rupture associated with historical earthquakes in the lower tagus valley, portugal. implications for seismic hazard in the greater lisbon area
publisher Frontiers Media S.A.
series Frontiers in Earth Science
issn 2296-6463
publishDate 2021-03-01
description The Lower Tagus Valley Fault, Portugal, has long been associated with the damaging earthquakes that affected the Greater Lisbon Area in historical times. These include a poorly documented earthquake that occurred in 1344, the relatively well-documented 1531 earthquake, and the most recent M6.0 1909 earthquake. In this work, we use a 0.5 m resolution LiDAR-based digital elevation model and a 0.5 cm resolution digital surface model based on UAV photogrammetry to accurately locate the fault scarps in the northernmost portion of the western fault strand and to select sites to perform paleoseimolological investigations. The paleoseismological and geochronological analysis performed in the Alviela trench site document the fault activity in the last 3000 years, including two earthquakes during historical times. We performed ground motion scenarios for 20 km, 40 km, and 60 km ruptures including the trench site. The ground motion fields obtained for the 40 km and 60 km ruptures are in agreement with most macroseismic intensity data available for the 1531 earthquake, implying a magnitude in the range M6.8–7.4. However, the degree of deformation preserved in the trench suggests a value closer to the lower magnitude bound. The intensity level observed in Lisbon in 1531 (IX) is lower than the modeled intensities for all considered scenarios and could be related to a particularly high level of vulnerability of the building stock.
topic lower Tagus valley fault zone
Lisbon 1531 earthquake
active faulting
paleoseismology trenching
ground motion scenarios
macroseismic intensity
url https://www.frontiersin.org/articles/10.3389/feart.2021.620778/full
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