Relaciones estratigrafías y sintectónicas de los conglomerados miocenos de Montejo de la Vega (borde SE de la cuenca del Duero)

Abstract

New precisions are given about the stratigraphy and chronology of the marginal conglomerate units and their associated distal fades in the SE sector of the Duero Basin are described. The syntectonic units formed during the latest episodes of Alpine uplift (Guadarrama stage) in Honrubia anticline located in the northern border fault of the Spanish Central System