Comment on “Integrated multi-stratigraphic study of the Coll de Terrers late Permian–Early Triassic continental succession from the Catalan Pyrenees (NE Iberian Peninsula): A geologic reference record for equatorial Pangaea” by Eudald Mujal, Josep Fortuny, Jordi Pérez-Cano, Jaume Dinarès-Turell, Jordi Ibáñez-Insa, Oriol Oms, Isabel Vila, Arnau Bolet, Pere Anadón. Global and Planetary Change 159 (2017) 46–60

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dc.contributor.authorRonchi, Ausonio
dc.contributor.authorLloret, Joan
dc.contributor.authorGretter, Nicola
dc.contributor.authorLópez Gómez, José
dc.contributor.authorHorra Del Barco, Raúl De La
dc.contributor.authorBarrenechea, José F.
dc.contributor.authorArche, Alfredo
dc.date.accessioned2023-06-17T13:20:38Z
dc.date.available2023-06-17T13:20:38Z
dc.date.issued2019-03
dc.description.abstractIn their paper, Mujal et al. (2017) describe as exceptional a section in the E Pyrenees (namely the Coll de Terrers), considering it a continental succession that continuously spans in time from the Late Permian to the Early Triassic. These authors describe the sandy-clayey red-beds of the upper Buntsandstein unit as the upper part of the Upper Red Unit (URU) and provide substantial stratigraphic and sedimentological data as well as palaeontological and mineralogical data in support of their thesis. We firstly have to consider that the post-Variscan deformation events altered the sedimentary contacts among the units (i.e. subsidence and tectonic evolution of the related sub-basins); and secondly, that the entire succession contains several tectonic structures affecting the late Palaeozoic-early Mesozoic sequence, due to the Alpine orogeny. The purported stratigraphic continuity between the Permian and Triassic is thus hampered not only by a different sedimentological and stratigraphical content but also by a complex tectonic framework.
dc.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/54667
dc.identifier.doi10.1016/j.gloplacha.2018.06.010
dc.identifier.issn0921-8181, ESSN: 1872-6364
dc.identifier.officialurlhttps://www.sciencedirect.com/science/article/pii/S0921818118301760
dc.identifier.urihttps://hdl.handle.net/20.500.14352/13165
dc.journal.titleGlobal and Planetary Change
dc.language.isoeng
dc.page.final179
dc.page.initial172
dc.publisherElsevier
dc.rights.accessRightsrestricted access
dc.subject.cdu551.75(234.12)
dc.subject.keywordPermian-Triassic transition
dc.subject.keywordStratigraphy
dc.subject.keywordWestern Tethys
dc.subject.keywordContinental facies
dc.subject.keywordPyrenees
dc.subject.ucmGeodinámica
dc.subject.ucmGeología estratigráfica
dc.subject.ucmPetrología
dc.subject.unesco2507 Geofísica
dc.subject.unesco2506.19 Estratigrafía
dc.titleComment on “Integrated multi-stratigraphic study of the Coll de Terrers late Permian–Early Triassic continental succession from the Catalan Pyrenees (NE Iberian Peninsula): A geologic reference record for equatorial Pangaea” by Eudald Mujal, Josep Fortuny, Jordi Pérez-Cano, Jaume Dinarès-Turell, Jordi Ibáñez-Insa, Oriol Oms, Isabel Vila, Arnau Bolet, Pere Anadón. Global and Planetary Change 159 (2017) 46–60
dc.typejournal article
dc.volume.number174
dspace.entity.typePublication
relation.isAuthorOfPublication509bf5dc-e657-4052-8eca-019bb7e1350b
relation.isAuthorOfPublication.latestForDiscovery509bf5dc-e657-4052-8eca-019bb7e1350b
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