English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/31522
Share/Impact:
Statistics
logo share SHARE logo core CORE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:

DC FieldValueLanguage
dc.contributor.authorSanz de Galdeano, Carlos-
dc.contributor.authorShanov, Stefan-
dc.contributor.authorGalindo-Zaldívar, Jesús-
dc.contributor.authorRadulov, Alexander-
dc.contributor.authorNikolov, Gabriel-
dc.date.accessioned2011-01-25T14:14:52Z-
dc.date.available2011-01-25T14:14:52Z-
dc.date.issued2010-08-
dc.identifier.citationJournal of Geodynamics 50(2): 57-66 (2010)es_ES
dc.identifier.issn0264-3707-
dc.identifier.urihttp://hdl.handle.net/10261/31522-
dc.description10 páginas, 8 figuras, 1 tabla.es_ES
dc.description.abstractIn the Tabernas Desert, a Neogene basin situated in SE Spain, major E-W folds coexist with large E-W dextral faults and abundant NNW-SSE faults. These faults affect the Plio-Quaternary sediments. The palaeostress ellipsoids indicate a roughly constant tension (σ3 axe) in the ENE-WSW direction, coexisting with a changeable direction of the main compression (σ1 axe) from the vertical to the NW-SE direction. The numerous NNW-SSE faults in southern areas, directly to the east of the city of Almería, tend to propagate northwards, forming a tectonic discontinuity of the Betic Internal Zone. The 2002 seismic swarm of the Gergal earthquake occurred in this NNW-SSE fault zone. In this setting, the E-W fractures act as transfer faults.es_ES
dc.description.sponsorshipThis study has been financed by the projects 2005BG0018 (CSIC—Bulgarian Academy of Sciences), CICYT CSD2006-00041, CGL2007-60535, CGL2009-07721, Junta de Andalucía P06RNM- 01521, 83/2007 (M.M.A.) and Groups RNM-024 and RNM-148.es_ES
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.rightsclosedAccesses_ES
dc.subjectBetic Cordilleraes_ES
dc.subjectNormal faultses_ES
dc.subjectStrike-slip faultses_ES
dc.subjectPaleostresses_ES
dc.subjectEarthquakeses_ES
dc.titleA new tectonic discontinuity in the Betic Cordillera deduced from active tectonics and seismicity in the Tabernas Basines_ES
dc.typeartículoes_ES
dc.identifier.doi10.1016/j.jog.2010.02.005-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.1016/j.jog.2010.02.005es_ES
Appears in Collections:(IACT) Artículos
Files in This Item:
There are no files associated with this item.
Show simple item record
 

Related articles:


WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.