Moreno Garrido, María CarmenSierra del Pino, SoniaSáez Ramos, Reinaldo2017-06-062017-06-061994http://hdl.handle.net/10272/13792Detrital platform sedimentation during the Devonian times took place in the homogeneous basin of the Iberian Pyrite Belt. This shallow basin changed to a mosaic of horsts and grabens just in the Devonian-Carboniferous boundary. Thick mattrix supported conglomerates (mega-debris flow) appear related with this dynamic. They suggest convulsive seismic events related to the Breton phase of the Hercynian orogenyspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/DevonianMega-debris flowIberian Pyrite Beltjournal articleopen access