Travertinos ligados a fallas: ejemplos del desierto de Tabernas (Almería, Cordillera Bética)

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dc.contributor.authorSanz de Galdeano, Carlos
dc.contributor.authorGalindo Zaldívar, Jesús
dc.contributor.authorMorales, Salvador
dc.contributor.authorLópez Chicano, Manuel
dc.contributor.authorAzañón, José Miguel
dc.contributor.authorMartín Rosales, Wenceslao
dc.date.accessioned2014-05-29T10:09:50Z
dc.date.available2014-05-29T10:09:50Z
dc.date.issued2008
dc.description.abstractIn the Tabernas desert there are several sectors with Quaternary travertines not formed in the proximities of carbonatic rocks, but originated by the rise of deep mineralized water along faults. These travertines have Fe mineralization in its older levels. The mineralization present similitude with that formed in the region during the late Miocene, then connected with the volcanismen_US
dc.identifier.urihttp://hdl.handle.net/10272/8203
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRightsopen access
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherTravertinesen_US
dc.subject.otherFaultsen_US
dc.subject.otherQuaternaryen_US
dc.subject.otherFe mineralizationen_US
dc.titleTravertinos ligados a fallas: ejemplos del desierto de Tabernas (Almería, Cordillera Bética)en_US
dc.titleTravertines linked to faults. Examples from the Tabernas desert (Almeria, Betic Cordillera)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 45, (2008)