Nota sobre la edad y posición tectónica de los conglomerados eocenos de Queralt (Prepirineo oriental, Prov. de Barcelona)
AbstractThe Eocene section of Queralt in the Spanish East Pyrenees (Prov. of Barcelona) is described. The Queralt conglomerates are defined as a marine slope deposit with interstratified mud flow beds. Their age is midle or uper Cuisian at the boton and Lutecian at the top. The tectonic phase of Pedraforca nappe was in the Lower Lutecian to Lower Biarritzian, and the nappe is covered by unconfortning beds of Biarritzian age.