Active deformation in old oceanic lithosphere and significance for earthquake hazard: Seismic imaging of the Coral Patch Ridge area and neighboring abyssal plains (SW Iberian Margin)
Martínez-Loriente, S. ... et al.-- 26 pages, 13 figures, 1 table
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Format: | artículo biblioteca |
Language: | English |
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American Geophysical Union
2013-07
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Subjects: | Multichannel seismics, Blind thrusts, Strike-slip faults, Seismic hazard assessment, Iberia-Africa boundary, Fault-bend folds, |
Online Access: | http://hdl.handle.net/10261/86986 |
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dig-icm-es-10261-869862020-11-10T10:42:35Z Active deformation in old oceanic lithosphere and significance for earthquake hazard: Seismic imaging of the Coral Patch Ridge area and neighboring abyssal plains (SW Iberian Margin) Martínez-Loriente, S. Gràcia, Eulàlia Bartolomé, Rafael Sallarès, Valentí Perea, Héctor Lo Iacono, Claudio Dañobeitia, Juan José Multichannel seismics Blind thrusts Strike-slip faults Seismic hazard assessment Iberia-Africa boundary Fault-bend folds Martínez-Loriente, S. ... et al.-- 26 pages, 13 figures, 1 table Recently acquired high-resolution multichannel seismic profiles together with bathymetric and sub-bottom profiler data from the external part of the Gulf of Cadiz (Iberia-Africa plate boundary) reveal active deformation involving old (Mesozoic) oceanic lithosphere. This area is located 180 km offshore the SW Iberian Peninsula and embraces the prominent NE-SW trending Coral Patch Ridge, and part of the surrounding deep Horseshoe and Seine abyssal plains. E-W trending dextral strike-slip faults showing surface deformation of flower-like structures predominate in the Horseshoe Abyssal Plain, whereas NE-SW trending compressive structures prevail in the Coral Patch Ridge and Seine Hills. Although the Coral Patch Ridge region is characterized by subdued seismic activity, the area is not free from seismic hazard. Most of the newly mapped faults correspond to active blind thrusts and strike-slip faults that are able to generate large magnitude earthquakes (Mw 7.2-8.4). This may represent a significant earthquake and tsunami hazard that has been overlooked so far. Key Points New active structures have been mapped in the Coral Patch Ridge area The newly mapped faults are able to generate large magnitude earthquakes (Mw>7) These new structures may represent a significant earthquake and tsunami hazard ©2013. American Geophysical Union. All Rights Reserved The authors acknowledge the support of the Spanish Ministry of Science and Innovation (MICINN) through National Projects EVENT (CGL2006–12861-C02-02) and SHAKE (CGL2011–30005-C02-02); the European Transnational Access SALVADORE program of the EU (RITA-CT-2004–505322), the ESF EuroMargins SWIM project (01- LEG-EMA09F and REN2002–11234E-MAR), the EU program ‘‘Global Change and Ecosystems’’ contract n. 037110 (NEAREST), the ESF TopoEurope TOPOMED project (CGL2008–03474-E/BTE), and the SWIMGLO project (PTDC/MAR/100522/2008). We also acknowledge funding from the MICINN through the ‘‘Ramon y Cajal’’ program (R. Bartolome) and from the CSIC through a JAE Pre-Doc fellowship (S. Martínez-Loriente) Peer Reviewed 2013-11-19T08:19:17Z 2013-11-19T08:19:17Z 2013-07 2013-11-19T08:19:17Z artículo http://purl.org/coar/resource_type/c_6501 doi: 10.1002/ggge.20173 issn: 1525-2027 Geochemistry, Geophysics, Geosystems 14(7): 2206-2231 (2013) http://hdl.handle.net/10261/86986 10.1002/ggge.20173 en https://doi.org/10.1002/ggge.20173 open American Geophysical Union |
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Multichannel seismics Blind thrusts Strike-slip faults Seismic hazard assessment Iberia-Africa boundary Fault-bend folds Multichannel seismics Blind thrusts Strike-slip faults Seismic hazard assessment Iberia-Africa boundary Fault-bend folds |
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Multichannel seismics Blind thrusts Strike-slip faults Seismic hazard assessment Iberia-Africa boundary Fault-bend folds Multichannel seismics Blind thrusts Strike-slip faults Seismic hazard assessment Iberia-Africa boundary Fault-bend folds Martínez-Loriente, S. Gràcia, Eulàlia Bartolomé, Rafael Sallarès, Valentí Perea, Héctor Lo Iacono, Claudio Dañobeitia, Juan José Active deformation in old oceanic lithosphere and significance for earthquake hazard: Seismic imaging of the Coral Patch Ridge area and neighboring abyssal plains (SW Iberian Margin) |
description |
Martínez-Loriente, S. ... et al.-- 26 pages, 13 figures, 1 table |
format |
artículo |
topic_facet |
Multichannel seismics Blind thrusts Strike-slip faults Seismic hazard assessment Iberia-Africa boundary Fault-bend folds |
author |
Martínez-Loriente, S. Gràcia, Eulàlia Bartolomé, Rafael Sallarès, Valentí Perea, Héctor Lo Iacono, Claudio Dañobeitia, Juan José |
author_facet |
Martínez-Loriente, S. Gràcia, Eulàlia Bartolomé, Rafael Sallarès, Valentí Perea, Héctor Lo Iacono, Claudio Dañobeitia, Juan José |
author_sort |
Martínez-Loriente, S. |
title |
Active deformation in old oceanic lithosphere and significance for earthquake hazard: Seismic imaging of the Coral Patch Ridge area and neighboring abyssal plains (SW Iberian Margin) |
title_short |
Active deformation in old oceanic lithosphere and significance for earthquake hazard: Seismic imaging of the Coral Patch Ridge area and neighboring abyssal plains (SW Iberian Margin) |
title_full |
Active deformation in old oceanic lithosphere and significance for earthquake hazard: Seismic imaging of the Coral Patch Ridge area and neighboring abyssal plains (SW Iberian Margin) |
title_fullStr |
Active deformation in old oceanic lithosphere and significance for earthquake hazard: Seismic imaging of the Coral Patch Ridge area and neighboring abyssal plains (SW Iberian Margin) |
title_full_unstemmed |
Active deformation in old oceanic lithosphere and significance for earthquake hazard: Seismic imaging of the Coral Patch Ridge area and neighboring abyssal plains (SW Iberian Margin) |
title_sort |
active deformation in old oceanic lithosphere and significance for earthquake hazard: seismic imaging of the coral patch ridge area and neighboring abyssal plains (sw iberian margin) |
publisher |
American Geophysical Union |
publishDate |
2013-07 |
url |
http://hdl.handle.net/10261/86986 |
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