Middle-Upper Triassic successions in the eastern Iberian Chain (Alt Palància and Manzanera areas): Stratigraphic precisions.
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...
| Authors: | , , , |
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| Format: | article |
| Status: | Published version |
| Publication Date: | 2021 |
| Country: | España |
| Institution: | Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya) |
| Repository: | Recercat. Dipósit de la Recerca de Catalunya |
| OAI Identifier: | oai:recercat.cat:2445/184724 |
| Online Access: | https://hdl.handle.net/2445/184724 |
| Access Level: | Open access |
| Keyword: | Estratigrafia Triàsic Serralada Ibèrica Stratigraphic geology Triassic Period Iberian Mountains |
| Summary: | 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. |
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