000148162 001__ 148162
000148162 005__ 20250120150146.0
000148162 0247_ $$2doi$$a10.1016/j.tecto.2015.05.025
000148162 0248_ $$2sideral$$a91411
000148162 037__ $$aART-2015-91411
000148162 041__ $$aeng
000148162 100__ $$0(orcid)0000-0003-0900-1440$$aEzquerro, L.$$uUniversidad de Zaragoza
000148162 245__ $$aSeismites from a well core of palustrine deposits as a tool for reconstructing the palaeoseismic history of a fault
000148162 260__ $$c2015
000148162 5060_ $$aAccess copy available to the general public$$fUnrestricted
000148162 5203_ $$aThe Concud Fault is located at the junction between the Jiloca and Teruel grabens (central-eastern Iberian Chain, Spain). The Late Pleistocene activity of this fault has been well logged from structural and palaeoseismological trench studies, but only scattered data of the Late Pliocene seismic activity exist. The Late Pliocene–Early Pleistocene syn-tectonic infill consists of an endorheic continental succession in which a 75 m-long continuous well was drilled near the Concud Fault. Along the entire well core, several types of soft-sediment deformation structures with variable morphology, size and frequency have occurred including clastic dykes, load structures and slumps. The rigorous analysis of the deformation structures, their relationships with the involved sedimentary facies, and the discrimination of possible deformation mechanisms and trigger processes allow us to interpret part of them as seismically-induced structures. The recognition of 21 deformed beds (seismites) allow the Late Pliocene–Early Pleistocene seismic history of the Concud Fault to be reconstructed. Therefore, 21 seismic events (with M ≥ 5) and an apparent recurrence period of about 45 ka have been inferred.
000148162 536__ $$9info:eu-repo/grantAgreement/ES/MINECO/BES-2010-031339$$9info:eu-repo/grantAgreement/ES/MINECO/CGL2012-35662
000148162 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc-nd$$uhttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
000148162 590__ $$a2.65$$b2015
000148162 591__ $$aGEOCHEMISTRY & GEOPHYSICS$$b23 / 81 = 0.284$$c2015$$dQ2$$eT1
000148162 592__ $$a1.918$$b2015
000148162 593__ $$aGeophysics$$c2015$$dQ1
000148162 593__ $$aEarth-Surface Processes$$c2015$$dQ1
000148162 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/acceptedVersion
000148162 700__ $$aMoretti, M.
000148162 700__ $$0(orcid)0000-0002-9130-117X$$aLiesa, C. L.$$uUniversidad de Zaragoza
000148162 700__ $$0(orcid)0000-0002-8929-9429$$aLuzón, A.$$uUniversidad de Zaragoza
000148162 700__ $$0(orcid)0000-0003-1412-5245$$aSimón, J. L.$$uUniversidad de Zaragoza
000148162 7102_ $$12000$$2428$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Geodinámica Interna
000148162 7102_ $$12000$$2280$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Estratigrafía
000148162 773__ $$g655 (2015), 191-205$$pTectonophysics$$tTectonophysics$$x0040-1951
000148162 8564_ $$s1443710$$uhttps://zaguan.unizar.es/record/148162/files/texto_completo.pdf$$yVersión publicada
000148162 8564_ $$s1351437$$uhttps://zaguan.unizar.es/record/148162/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000148162 909CO $$ooai:zaguan.unizar.es:148162$$particulos$$pdriver
000148162 951__ $$a2025-01-20-14:59:37
000148162 980__ $$aARTICLE