Please use this identifier to cite or link to this item:
Full metadata record
DC FieldValueLanguage
dc.contributor.authorAsensio Ferreira, Eva-
dc.contributor.authorKhazaradze, Giorgi-
dc.contributor.authorEcheverria Moreno, Ana-
dc.contributor.authorKing, R. W.-
dc.contributor.authorVilajosana Guillén, Ignasi-
dc.description.abstractThe Pyrenees mountain belt, which separates the Iberian Peninsula from the rest of the European continent, is part of the Alpine<br>Himalayan orogenic belt, formed as a result of a collision between the African and Eurasian Plates. Although the instrumental seismicity in the Pyrenees is moderate, in the past centuries a number of destructive earthquakes have occurred, which could indicate continuing tectonic activity of the area. We analyse GPS observations spanning 3.5 yr from 35 continuous stations in the Pyrenees region and find significant on-going extension perpendicular to the range at 2.5 ± 0.5 nstrain yr<br>1, with the possibility of higher strain rates concentrated in the westernmost part of the range. This finding is in agreement with the predominantly normal faulting focal mechanisms of earthquakes that occur in the area and suggests a recurrence time for magnitude 6.5 earthquakes of 2200<br>2500 yr.-
dc.format.extent9 p.-
dc.publisherRoyal Astronomical Society-
dc.relation.isformatofReproducció del document publicat a: 10.1111/j.1365-246X.2012.05525.x-
dc.relation.ispartofGeophysical Journal International, 2012, vol. 190, num. 2, p. 913-921-
dc.rights(c) Asensio Ferreira, Eva et al., 2012-
dc.subject.classificationSistema de posicionament global-
dc.subject.otherGlobal Positioning System-
dc.titleGPS studies of active deformation in the Pyrenees-
Appears in Collections:Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)

Files in This Item:
File Description SizeFormat 
592184.pdf6.33 MBAdobe PDFView/Open

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.