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dc.contributor.author | Sànchez-Serra, Cristina | - |
dc.contributor.author | Gràcia, Eulàlia | - |
dc.contributor.author | Bartolomé, Rafael | - |
dc.contributor.author | Martínez-Loriente, S. | - |
dc.contributor.author | Perea, Héctor | - |
dc.contributor.author | Lo Iacono, Claudio | - |
dc.contributor.author | Sallarès, Valentí | - |
dc.contributor.author | Urgeles, Roger | - |
dc.date.accessioned | 2018-10-30T10:32:36Z | - |
dc.date.available | 2018-10-30T10:32:36Z | - |
dc.date.issued | 2018-06 | - |
dc.identifier | isbn: 978-84-09-02473-5 | - |
dc.identifier.citation | Iberfault 2018 : Avances en el estudio de Fallas Activas, Terremotos y Peligrosidad Sísmica de Iberia : III Reunión Ibérica sobre Fallas Activas y Paleosismología : Volumen de resúmenes: 321-324 (2018) | - |
dc.identifier.uri | http://hdl.handle.net/10261/171730 | - |
dc.description | Inciativa Ibérica para el Estudio de las Fallas Activas, Tercera Reunión Ibérica sobre Fallas Activas y Paleosismología IBERFAULT 2018 - Third Iberian Meeting on Active Faults and Paleoseismology, 11-13 June 2018, Alicante, Spain.-- 4 pages, 4 figures | - |
dc.description.abstract | The Gulf of Cadiz is located at the SW Iberian Margin and hosts the African-Eurasian plate boundary. This is one of the most seismogenic areas in Western Europe, where historical and instrumental earthquakes occurred, ranging from Mw 6 to 8.5, and some of them triggered destructive tsunamis. The ICM-CSIC team keeps investigating the Gulf of Cadiz area since more than 15 years, carrying out multiscale bathymetric, high-resolution to deep seismic and sampling surveys. The active structures in the Gulf of Cadiz can be classified in two main families: The WNW-ESE dextral strike-slip faults and the NE-SW thrusts faults. The orientation of these faults is compatible with the current plate convergence in the region. The largest active strike-slip faults are: -the Lineament South and the Lineament North that may generate earthquakes up to Mw 8; while the active NE-SW thrust faults, the Marquês de Pombal, the Horseshoe and the Coral Patch Ridge faults can individually generate earthquakes up to Mw7.8 | - |
dc.rights | openAccess | - |
dc.subject | Earthquakes tsunamis | - |
dc.subject | Reverse faults | - |
dc.subject | Strike-slip faults | - |
dc.subject | Gulf of Cadiz | - |
dc.title | Hazard in the Gulf of Cadiz: review of the large seismogenic structures | - |
dc.title.alternative | Peligrosidad en el Golfo de Cádiz: Revisión de las principales estructuras sismogénicas | - |
dc.type | comunicación de congreso | - |
dc.date.updated | 2018-10-30T10:32:36Z | - |
dc.description.version | Peer Reviewed | - |
dc.language.rfc3066 | eng | - |
dc.relation.csic | Sí | - |
dc.type.coar | http://purl.org/coar/resource_type/c_5794 | es_ES |
item.grantfulltext | open | - |
item.fulltext | With Fulltext | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.cerifentitytype | Publications | - |
item.openairetype | comunicación de congreso | - |
Aparece en las colecciones: | (ICM) Comunicaciones congresos |
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Serra_et_al_ 2018.pdf | 594,74 kB | Adobe PDF | Visualizar/Abrir |
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