@article{10272/20542,
year = {2021},
url = {http://hdl.handle.net/10272/20542},
abstract = {Se describe un cabalgamiento cuaternario, que corta a una brecha sedimentaria que recubre la terraza de +5 m del río Ibor, en el
extremo occidental de los Montes de Toledo. El sistema de cabalgamientos descrito ha condicionado la localización de abanicos aluviales fini-neógenos (“raña”), por lo que ha de considerarse como activo
durante los últimos 9 Ma. El sismo asociado, superficial, se estima de
una magnitud entre M 6-6.5. La rotura se localiza a menos de 20 km
de la Central Nuclear de Almaraz (Cáceres)},
abstract = {A Quaternary overthrust is described, intersecting a sedimentary
breccia covering the +5 m terrace of the Ibor River, at the western
end of the Montes de Toledo. The resulting thrusting system has
conditioned the location of fini-neogene alluvial fans ("raña"), so it
has to be considered as active during the last 9 Ma. The associated, superficial earthquake is estimated to range between M 6-6.5 in
magnitude. The rupture is located less than 20 km from the Almaraz
Nuclear Power Plant (Cáceres)},
publisher = {Sociedad Geológica de España},
title = {El Cabalgamiento de El Ibor: una falla cuaternaria a 20 km de la Central Nuclear de Almaraz},
title = {The Ibor Thrust: a quaternary fault 20 km from the Almaraz Nuclear Power Plant},
author = {Vicente, Gerardo de and Díez Fernández, Rubén},
}