dc.contributor.author
Ortí Cabo, Federico
dc.contributor.author
Guimerà i Rosso, Joan J.
dc.contributor.author
Benedicto, C.
dc.contributor.author
Pérez-López, A.
dc.date.issued
2022-04-07T07:28:20Z
dc.date.issued
2022-04-07T07:28:20Z
dc.date.issued
2022-04-07T07:28:20Z
dc.identifier
https://hdl.handle.net/2445/184724
dc.description.abstract
Cartographic, 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.
dc.format
application/pdf
dc.publisher
Sociedad Geológica de España
dc.relation
Reproducció del document publicat a: https://sge.usal.es/archivos/GEO_TEMAS/Geo_temas18.pdf
dc.relation
Geo-Temas, 2021, vol. 18, p. 174-177
dc.rights
(c) Sociedad Geológica de España, 2021
dc.rights
info:eu-repo/semantics/openAccess
dc.source
Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)
dc.subject
Serralada Ibèrica
dc.subject
Stratigraphic geology
dc.subject
Triassic Period
dc.subject
Iberian Mountains
dc.title
Middle-Upper Triassic successions in the eastern Iberian Chain (Alt Palància and Manzanera areas): Stratigraphic precisions.
dc.type
info:eu-repo/semantics/article
dc.type
info:eu-repo/semantics/publishedVersion
