Precisiones sobre la cinemática y edad de la falla del Río de la Miel (Maro, Málaga)

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dc.contributor.authorPérez Ramos, Isaac
dc.contributor.authorSanz de Galdeano, Carlos
dc.contributor.authorAndreo Navarro, Bartolomé
dc.contributor.authorPistre, S.
dc.date.accessioned2014-10-23T09:05:03Z
dc.date.available2014-10-23T09:05:03Z
dc.date.issued2004
dc.description.abstractThe Río de la Miel fault shows a complex movement history. Three main displacement stages have been distinguished from the microtectonic analysis. The first stage was a dextral strike-slip movement whose cr, was almost horizontal with, a NNW-SSE direction. The second stage was a normal movemént with cr, situated in the vertical. Finally, in the third stage, cr, had a low dipping angle and a NNE-SSW direction. The vertical displacement of the fault reach several hundreds of metres, probably more than 500. m. This fault has been active at least during the lower Plioceneen_US
dc.identifier.urihttp://hdl.handle.net/10272/8953
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherRío de la Mielen_US
dc.subject.otherSierra Almijaraen_US
dc.subject.otherStrike-slip faultsen_US
dc.subject.otherNormal faultsen_US
dc.titlePrecisiones sobre la cinemática y edad de la falla del Río de la Miel (Maro, Málaga)en_US
dc.titleCinematic and age remarks on the Río de la Miel fault (Maro, Málaga)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 36, (2004)