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dc.contributor.authorFlores, E.-
dc.contributor.authorRodríguez Vidal, Joaquín-
dc.contributor.authorCáceres Puro, L.-
dc.date.accessioned2013-06-06T10:01:59Z-
dc.date.available2013-06-06T10:01:59Z-
dc.date.issued1993-
dc.identifier.citationGeogaceta 14: 123-125 (1993)es_ES
dc.identifier.issn0213-683X-
dc.identifier.urihttp://hdl.handle.net/10261/77705-
dc.description3 páginas, 1 figura, 9 referencias.-- 15ª Sesión Científica, Fuengirola, Málaga, 1993.es_ES
dc.description.abstractThe end of the Pliocene was characterized by a return to the compressive regime throughout the southern of the Iberian peninsula. Quaternary deformations are intense in places and correspond to folds and occasionally reversal faults. At the western sector of the Guadalquivir basin the neotectonic activity is not still investigated. The studied section shows folded Quaternary terrace deposits and sometimes crushed terraces between mesozoic rack bodies. The entire studied outcrop looks as a WSW-ENE/W-E fault zone that, also a possible previous activity, it would support strain, at least compressive, contemporary to the terrace deposits (Pleistocene).es_ES
dc.description.sponsorshipEste trabajo ha sido subvencionado por el proyecto de la DGICYT; PB91- 0622. Es una contribución al IGCP-274 y al Grupo de Investigación 4079 de la Junta de Andalucía.es_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsopenAccesses_ES
dc.subjectNeotectonicses_ES
dc.subjectQuaternaryes_ES
dc.subjectGuadalquivir basines_ES
dc.subjectAlgarvees_ES
dc.titleNuevos datos sobre comprensión pleistocena en el extremo oriental del Algarve (Portugal)es_ES
dc.typeartículoes_ES
dc.description.peerreviewedPeer reviewedes_ES
dc.contributor.funderDirección General de Investigación Científica y Técnica, DGICT (España)-
dc.identifier.funderhttp://dx.doi.org/10.13039/501100008737es_ES
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