Barea, JoséLópez Martínez, JerónimoDurán Valsero, Juan JoséArribas, A.Julià, Ramón2014-12-092014-12-092001http://hdl.handle.net/10272/9487Geomorphological, sedimentological and palaeontological evidences allowed to identify several phases in the evolution of the Patones-Cerro c/e la Oliva karstic massif. The studied speleothems, jointly with data of previous works indicate the presence of at least five episodes of chemical precipitation under favorable climatic conditions during isotopic stages 9-11?, 7, 5, 4-3 and 7, respectivelyspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/KarstEvolución paleoambientalCuaternarioSistema Centraljournal articleopen access