Martínez Poyatos, DavidSimancas Cabrera, J. F.Azor, A.2015-02-032015-02-032000http://hdl.handle.net/10272/9783In the southern part of the Central Iberian Zone (Iberian Massif), a Lower Carboniferous thrust superposed to the NE an allochthonous unit onto a paraautochthonous one. In the Espiel area, the thrust geometry includes several frontal horses. Furthermore, lateral confining of the nappe during transport produced a lateral hanging wall slice that branches out from the main thrust in the location of a lateral hanging wall rampspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Thrust geometryLateral imbricationSouthern Central Iberian ZoneVariscan Beltjournal articleopen access