@article{10272/8599,
year = {2006},
url = {http://hdl.handle.net/10272/8599},
abstract = {We studied various Upper Miocene (Turolian) layers of superimposed soft-sediment deformation structures
induced by liquefaction in the Granada basin (Betic Cordillera). These are principally load structures:
sagging and dome load casts, ball-and-pillow and drop structures. Based on analyses of their morphology
and of the facies, these have been interpreted as being the result of liquefaction of non-cohesive sediments
during earthquakes. The intense synsedimentary fracturing and the presence of seismites highlight the
strongly influence of tectonic activity in the Granada basin during the Late Miocene, with earthquakes of
moderate to high magnitude occurring which were capable of liquefying the sediment},
title = {Estructuras sedimentarias de deformación interpretadas como sismitas en el Mioceno Superior (Turoliense) de la cuenca de Granada (Cordillera Bética)},
title = {Soft-sediment deformation structures interpreted as seismites in the late Miocene (Turolian) of the Granada basin
(Betic Cordillera)},
author = {Alfaro García, Pedro and Galindo Zaldívar, Jesús and Jabaloy, A. and López Garrido, Ángel Carlos and Sanz de Galdeano, Carlos},
}