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The 1755 Lisbon earthquake and the beginning of closure of the Atlantic

Bibliographic Data

ID12417838
AuthorsA Ribeiro (0000-0003-4028-7897, corresponding author), L Mendes-Victor, João Cabral (0000-0003-4175-6835), Luís Matias (0000-0002-8086-4874), Pedro Terrinha (0000-0002-6824-6002)
Year2006
Volume14
Issue2
Pages193-205
Publication date2006-04-12
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEuropean Review (JOURNAL)
Journal identifiersISSN: 1062-7987 • E-ISSN: 1474-0575
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.1017/s1062798706000196
OpenAlexW2049074282
LanguageEN
Citations received3

The 1755 Lisbon earthquake and tsunami had one of the highest magnitudes in the history of Europe. The source mechanism requires generation at a subduction zone. Intensity distribution and tsunami modelling excludes the Gorringe Bank as a source area and suggests generation by the incipient convergence of the Atlantic with the Southwest Iberia and Morocco margin rather than at the less active Gulf of Cadiz Accretionary Prism. The comparison with the 2004 Sumatra earthquake and tsunami supports this interpretation. A tsunami warning alert system is urgent for the Atlantic

Accretionary wedge · Convergence zone · Margin (machine learning · Seismology · Subduction · Tectonics · Tsunami earthquake · earthquake and tectonic studies · Geological and Geochemical Analysis · Geological and Geophysical Studies Worldwide · Geology · Oceanography

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Unique citing works3
Citations per year0,75
Citation span2022 - 2024 (3)
Citation velocityrecent
Highly citedNo
Citation typesNeutral: 3

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