Calibración de la constante de difusión (k0) para la datación de escarpes cosísmicos: aplicación al terremoto de Alborax (Albacete, SE España)

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dc.book.titleContribuciones al Estudio del Periodo Cuaternario
dc.contributor.authorPérez López, Raúl
dc.contributor.authorRodríguez Pascua, Miguel Angel
dc.contributor.authorGiner Robles, Jorge Luis
dc.contributor.authorCalvo Sorando, José Pedro
dc.contributor.authorGarduño Monroy, V.H.
dc.contributor.authorIsrade Alcántara, I.
dc.contributor.authorBischoff, James L.
dc.contributor.editorLario Gómez, Javier
dc.contributor.editorSilva Barroso, Pablo Gabriel
dc.date.accessioned2024-03-13T14:46:53Z
dc.date.available2024-03-13T14:46:53Z
dc.date.issued2007
dc.description.abstractThe diffusion equation was formulated to estimate the age of fault scarps. This technique is rather simple, taking into account the degradation of the unconsolidated scarp with the time. The Tobarra-Cordovilla segment consists in a surface rupturing associated to undated paleoearthquakes. This segment configures a graben basin with normal faults affecting Quaternary deposits. Preliminary study of the paleoearthquake indicates a magnitude greater than 5.5. As a primary approach, we have applied the Diffusion Equation in order to delimitate the age interval of occurrence. However, the diffusion constant for such equation (K0) is only calibrated for arid environmental. Therefore, we have introduced a new equation to obtain the K0-value according the fault throw, the erodability and the apparent density of the unconsolidated faulted sediment.
dc.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedFALSE
dc.description.sponsorshipMinisterio de Educación y Ciencia
dc.description.statuspub
dc.identifier.isbn978-84-7484-201-2
dc.identifier.urihttps://hdl.handle.net/20.500.14352/102196
dc.language.isospa
dc.page.final162
dc.page.initial161
dc.page.total2
dc.publication.placeMadrid
dc.publisherEscuela Técnica Superior de Ingenieros Industriales de Madrid ; Universidad Politécnica de Madrid
dc.relation.projectIDMEC ACTISIS (CGL2006-05001-BTE)
dc.rights.accessRightsrestricted access
dc.subject.cdu550.34
dc.subject.cdu551.2
dc.subject.keywordescarpe de falla
dc.subject.keywordecuación de difusión
dc.subject.keyworddatación
dc.subject.keywordterremoto Alborax
dc.subject.keywordAlbacete
dc.subject.keywordfault scarp
dc.subject.keyworddiffusion equation
dc.subject.keyworddating techniques
dc.subject.keywordAlborax earthquake
dc.subject.keywordSpain
dc.subject.ucmGeodinámica
dc.subject.ucmSismología (Geología)
dc.subject.unesco2507 Geofísica
dc.titleCalibración de la constante de difusión (k0) para la datación de escarpes cosísmicos: aplicación al terremoto de Alborax (Albacete, SE España)
dc.title.alternativeCalibration of the diffusion constant (k0) for dating coseismic fault scarps by using the diffusion equation: application to the Alborax earthquake, Albacete, SW Spain)
dc.typebook part
dc.type.hasVersionVoR
dspace.entity.typePublication
relation.isAuthorOfPublicationac6d5176-a506-4777-9bd4-e8e44d895119
relation.isAuthorOfPublication4aa3824b-ca03-45fd-b468-ebd78cb1ac8f
relation.isAuthorOfPublication.latestForDiscoveryac6d5176-a506-4777-9bd4-e8e44d895119
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