Lillo Bevia, J.Oyarzun, RobertoOrtega, Lorena2017-02-242017-02-241995http://hdl.handle.net/10272/13389Sulphur isotope data from several base metals-Ba-(F)-(Ag) and Ag-base metals vein-type deposits in the Central Iberian Zone o f the Hesperian Massif suggest a magmatic and /or metasedimentary origin o f this ore-forming component. Deposits exclusively hosted in metasediments (p.e. Alcudia Valley, type IV) display a magmatic signature. Even those lodes and stratabound deposits hosted by Permian-Triassic terrigenous and andesites (Las Torrecillas-Linares y Atienza) are formed by "igneous" sulphurspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Pb-ZnAgVein-type mineralizationsSpanish Central SystemLinares-La CarolinaAlcudia ValleyCentral Iberian Zonejournal articleopen access