Ortí Cabo, FedericoGuimerà i Rosso, Joan J.Benedicto, C.Pérez-López, A.2022-04-072022-04-072021-071576-5172https://hdl.handle.net/2445/184724Cartographic, statigraphic and structural studies in the Alt Palància and Manzanera areas indicate that the Middle-Upper Triassic successions entirely belong to the 'Mediterranean type of Triassic'. The two carbonate units of the Muschelkalk facies have carbonate-marl alternations both at the base and at the top. The palynological study of claystones and marls allows dating the Röt facies and the three Mus-chelkalk units. The isotopic study of gypsum samples allows distinguishing the middle Muschelkalk unit from the Keuper unit despite the facies similarity and tectonic disruption.4 p.application/pdfeng(c) Sociedad Geológica de España, 2021EstratigrafiaTriàsicSerralada IbèricaStratigraphic geologyTriassic PeriodIberian Mountainsinfo:eu-repo/semantics/article7228262022-04-07info:eu-repo/semantics/openAccess