Determinación de la naturaleza de la falla de Cerro Tajo (Macizo peridotítico de Carratraca) mediante termocronología de trazas de fisión

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dc.contributor.authorEsteban, José Julián
dc.contributor.authorCuevas, Julia
dc.contributor.authorTubía, José María
dc.contributor.authorSeward, D.
dc.date.accessioned2014-10-21T11:55:03Z
dc.date.available2014-10-21T11:55:03Z
dc.date.issued2004
dc.description.abstractFission-track thermochronology has been applied to assess the nature of the tectonic contact of Cerro Tajo, near Carratraca (Málaga). Zircon fission-track ages support the idea of the extensional nature of the Cerro Tajo fault, coherent with its NW movement and the omission of materials. Apatite fission-track ages have helped to constraint the displacement of the fault to between 20 and 17 Ma, meanwhile the resetting of one sample located in the fault contact may be associated with heat liberated during a late fault reactivation, fluids circulation or serpentinizationen_US
dc.identifier.urihttp://hdl.handle.net/10272/8924
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.otherAlpujarride Complexen_US
dc.subject.otherLos Reales nappeen_US
dc.subject.otherFission-track thermochronologyen_US
dc.subject.otherTectonic contacten_US
dc.titleDeterminación de la naturaleza de la falla de Cerro Tajo (Macizo peridotítico de Carratraca) mediante termocronología de trazas de fisiónen_US
dc.titleAssessing the nature of the Cerro Tajo fault (Carratraca peridote massif) using fission-track thermochronologyeng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 36, (2004)