Sanz Rubio, E.Hoyos, M.Cañaveras, J.C.Sánchez Moral, S.Calvo, J. Pedro2016-04-082016-04-081996http://hdl.handle.net/10272/11824A complex fluviolacustrine calcareous system with associated autochtonous tufa deposits is recognized in the Upper Miocene-Pliocene of the Neogene Calatayud Basin. A detailed sedimentological analysis of the calcareous sediments reveals a wide spectrum óf facies associations mainly related to reworking of tufa deposits including products such as oncolithic tufas and less common phytoclastic and intraclastic tufasspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Calatayud BasinMiocene-PlioceneTufaOncoidsjournal articleopen access