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Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/184724
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dc.contributor.authorOrtí Cabo, Federico-
dc.contributor.authorGuimerà i Rosso, Joan J.-
dc.contributor.authorBenedicto, C.-
dc.contributor.authorPérez-López, A.-
dc.date.accessioned2022-04-07T07:28:20Z-
dc.date.available2022-04-07T07:28:20Z-
dc.date.issued2021-07-
dc.identifier.issn1576-5172-
dc.identifier.urihttp://hdl.handle.net/2445/184724-
dc.description.abstractCartographic, 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.extent4 p.-
dc.format.mimetypeapplication/pdf-
dc.language.isoeng-
dc.publisherSociedad Geológica de España-
dc.relation.isformatofReproducció del document publicat a: https://sge.usal.es/archivos/GEO_TEMAS/Geo_temas18.pdf-
dc.relation.ispartofGeo-Temas, 2021, vol. 18, p. 174-177-
dc.rights(c) Sociedad Geológica de España, 2021-
dc.sourceArticles publicats en revistes (Dinàmica de la Terra i l'Oceà)-
dc.subject.classificationEstratigrafia-
dc.subject.classificationTriàsic-
dc.subject.classificationSerralada Ibèrica-
dc.subject.otherStratigraphic geology-
dc.subject.otherTriassic Period-
dc.subject.otherIberian Mountains-
dc.titleMiddle-Upper Triassic successions in the eastern Iberian Chain (Alt Palància and Manzanera areas): Stratigraphic precisions.-
dc.typeinfo:eu-repo/semantics/article-
dc.typeinfo:eu-repo/semantics/publishedVersion-
dc.identifier.idgrec722826-
dc.date.updated2022-04-07T07:28:20Z-
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess-
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