ISSN (print): 1698-6180. ISSN (online): 1886-7995 www.ucm.es/info/estratig/journal.htm Journal of Iberian Geology 38 (1) 2012: 127-144 http://dx.doi.org/10.5209/rev_JIGE.2012.v38.n1.39209 Active extensional faults in the central-eastern Iberian Chain, Spain Fallas activas extensionales en la Cordillera Ibérica centro-oriental J.L. Simón*, L.E. Arlegui, P. Lafuente, C.L. Liesa Dpt. Ciencias de la Tierra, Facultad de Ciencias, Universidad de Zaragoza, c/ Pedro Cerbuna 12, E-50009 Zaragoza, Spain
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[email protected] *Corresponding author Received: 27/06/2011 / Accepted: 29/02/2012 Abstract Among the conspicuous extensional structures that accommodate the onshore deformation of the Valencia Trough at the central- eastern Iberian Chain, a number of large faults show evidence of activity during Pleistocene times. At the eastern boundary of the Jiloca graben, the Concud fault has moved since mid Pliocene times at an average rate of 0.07-0.08 mm/y, while rates from 0.08 to 0.33 mm/y have been calculated using distinct stratigraphic markers of Middle to Late Pleistocene age. A total of nine paleoseisms associated to this fault have been identified between 74.5 and 15 ka BP, with interseismic periods ranging from 4 to 11 ka, estimated coseismic displacements from 0.6 to 2.7 m, and potential magnitudes close to 6.8. The other master faults of the Jiloca graben (Ca- lamocha and Sierra Palomera faults) have also evidence of Pliocene to Late Pleistocene displacement, with average slip rates of 0.06 and 0.11-0.15 mm/y, respectively.