Zobrazeno 1 - 10
of 31
pro vyhledávání: '"Triàsic"'
Autor:
Andrey A. Gurenko, Jesús Solé, Carles Fabrega, David Parcerisa, Anna Travé, Médard Thiry, Christine Franke, David Gómez-Gras
Publikováno v:
Recercat. Dipósit de la Recerca de Catalunya
instname
UPCommons. Portal del coneixement obert de la UPC
Universitat Politècnica de Catalunya (UPC)
Dipòsit Digital de la UB
Universidad de Barcelona
instname
UPCommons. Portal del coneixement obert de la UPC
Universitat Politècnica de Catalunya (UPC)
Dipòsit Digital de la UB
Universidad de Barcelona
This is a post-peer-review, pre-copyedit version of an article published in International Journal of Earth Sciences. The final authenticated version is available online at: http://dx.doi.org/10.1007/s00531-019-01764-0. Extensive areas of the Variscan
Publikováno v:
Dipòsit Digital de la UB
Universidad de Barcelona
Universidad de Barcelona
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::7b02adf0414c27fcd26da85e6c8ba8e5
http://hdl.handle.net/2445/184724
http://hdl.handle.net/2445/184724
Publikováno v:
Recercat: Dipósit de la Recerca de Catalunya
Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
Ortí, F, Guimerà, J & Goetz, A E 2020, ' Middle-Upper Triassic stratigraphy and structure of the Alt Palància (eastern Iberian Chain): a multidisciplinary approach ', Geologica Acta, vol. 18, 4 . https://doi.org/10.1344/GeologicaActa2020.18.4
Dipòsit Digital de la UB
Universidad de Barcelona
Dipòsit Digital de Documents de la UAB
Universitat Autònoma de Barcelona
Recercat. Dipósit de la Recerca de Catalunya
instname
Geologica Acta; Vol. 18 (2020); 1-26, I-II
RCUB. Revistas Científicas de la Universidad de Barcelona
Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
Ortí, F, Guimerà, J & Goetz, A E 2020, ' Middle-Upper Triassic stratigraphy and structure of the Alt Palància (eastern Iberian Chain): a multidisciplinary approach ', Geologica Acta, vol. 18, 4 . https://doi.org/10.1344/GeologicaActa2020.18.4
Dipòsit Digital de la UB
Universidad de Barcelona
Dipòsit Digital de Documents de la UAB
Universitat Autònoma de Barcelona
Recercat. Dipósit de la Recerca de Catalunya
instname
Geologica Acta; Vol. 18 (2020); 1-26, I-II
RCUB. Revistas Científicas de la Universidad de Barcelona
The present study provides new data of the Middle-Upper Triassic successions and their deformation in the eastern Iberian Chain, where contractional tectonics during the Cenozoic disrupted this Mediterranean type of Triassic rocks. The succession, di
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9f62e844ce7bf2e3a1d4e51ac7d22c24
http://hdl.handle.net/2072/442778
http://hdl.handle.net/2072/442778
Autor:
Laura Rosell, Xavier Castelltort, M. Inglès, Federico Ortí, Elisabet Playà, Josep Maria Salvany
Publikováno v:
Recercat. Dipósit de la Recerca de Catalunya
instname
UPCommons. Portal del coneixement obert de la UPC
Universitat Politècnica de Catalunya (UPC)
instname
UPCommons. Portal del coneixement obert de la UPC
Universitat Politècnica de Catalunya (UPC)
The eastern sector of the epicontinental Iberian platform underwent restriction after the sedimentation of the lower Muschelkalk carbonates (Middle Triassic) under extensional regime. This resulted in the accumulation of the marine evaporites and the
Publikováno v:
UPCommons. Portal del coneixement obert de la UPC
Universitat Politècnica de Catalunya (UPC)
Recercat. Dipósit de la Recerca de Catalunya
instname
Universitat Politècnica de Catalunya (UPC)
Recercat. Dipósit de la Recerca de Catalunya
instname
This paper deals with the Middle Triassic-to-earliest Jurassic evaporite sedimentation in the epicontinental, eastern Iberian platform. This deposition occurred under extensional regime during the westwards migration of the Neotethys Ocean at the sta
Publikováno v:
Dipòsit Digital de la UB
Universidad de Barcelona
Universidad de Barcelona
A new actinopterygian, Moradebrichthys vilasecae gen. et sp. nov., from the Middle Triassic (Late Ladinian) of Móra d'Ebre-Camposines (Catalonia, NE Iberian Peninsula) is erected on the basis of several, almost complete, articulated and well-preserv
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4ce1285a1d103be6ef418a25b8803619
http://hdl.handle.net/2445/168813
http://hdl.handle.net/2445/168813
Autor:
Cristina Villanova-de-Benavent, Joaquín A. Proenza, Jingyao Xu, Montgarri Castillo-Oliver, Marc Campeny, Yael Díaz-Acha, Lisard Torró, Esperança Tauler, Sandra Amores-Casals, Joan Carles Melgarejo
Publikováno v:
RECERCAT (Dipòsit de la Recerca de Catalunya)
Recercat. Dipósit de la Recerca de Catalunya
instname
Minerals, Vol 10, Iss 1, p 34 (2019)
Recercat: Dipósit de la Recerca de Catalunya
Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
Dipòsit Digital de la UB
Universidad de Barcelona
Minerals
Volume 10
Issue 1
Recercat. Dipósit de la Recerca de Catalunya
instname
Minerals, Vol 10, Iss 1, p 34 (2019)
Recercat: Dipósit de la Recerca de Catalunya
Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
Dipòsit Digital de la UB
Universidad de Barcelona
Minerals
Volume 10
Issue 1
The Eureka deposit in Castell-estaó
in the Catalan Pyrenees is a Cu&ndash
U&ndash
V deposit, hosted by Triassic red-bed sandstones, and classified here as a low-temperature, sandstone-hosted stratabound metamorphite U deposit. Th
in the Catalan Pyrenees is a Cu&ndash
U&ndash
V deposit, hosted by Triassic red-bed sandstones, and classified here as a low-temperature, sandstone-hosted stratabound metamorphite U deposit. Th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6ac06b621e20ebbdc01dd0ff2b30108f
http://hdl.handle.net/2072/449872
http://hdl.handle.net/2072/449872
Autor:
Pere Anadón, Josep Fortuny, Jordi Ibáñez-Insa, Isabel Vila, Jordi Pérez-Cano, Eudald Mujal, Jaume Dinarès-Turell, Arnau Bolet, Oriol Oms
Publikováno v:
Recercat. Dipósit de la Recerca de Catalunya
instname
Global and Planetary Change
Global and Planetary Change, 2017, 159, pp.46-60. ⟨10.1016/j.gloplacha.2017.10.004⟩
Digital.CSIC. Repositorio Institucional del CSIC
Global and Planetary Change, Elsevier, 2017, 159, pp.46-60. ⟨10.1016/j.gloplacha.2017.10.004⟩
Dipòsit Digital de la UB
Universidad de Barcelona
instname
Global and Planetary Change
Global and Planetary Change, 2017, 159, pp.46-60. ⟨10.1016/j.gloplacha.2017.10.004⟩
Digital.CSIC. Repositorio Institucional del CSIC
Global and Planetary Change, Elsevier, 2017, 159, pp.46-60. ⟨10.1016/j.gloplacha.2017.10.004⟩
Dipòsit Digital de la UB
Universidad de Barcelona
The most severe biotic crisis on Earth history occurred during the Permian–Triassic (PT) transition around 252 Ma. Whereas in the marine realm such extinction event is well-constrained, in terrestrial settings it is still poorly known, mainly due t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4b4f15a710f5975b043367c51115e215
http://hdl.handle.net/10261/157289
http://hdl.handle.net/10261/157289
Autor:
Mercedes Martín, Ramón
Publikováno v:
TDX (Tesis Doctorals en Xarxa)
TDR. Tesis Doctorales en Red
instname
Dipòsit Digital de la UB
Universidad de Barcelona
TDR. Tesis Doctorales en Red
instname
Dipòsit Digital de la UB
Universidad de Barcelona
[spa] El registro sedimentario de la facies Muschelkalk superior (Triásico medio) de la Cuenca Catalana constituye un importante pulso transgresivo ladiniense en el NE de Iberia. Las curvas de subsidencia calculadas muestran dos etapas de subsidenci
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::5536f41df8c95aae43efb082a5c7c78c
http://hdl.handle.net/10803/132602
http://hdl.handle.net/10803/132602
Publikováno v:
Recercat. Dipósit de la Recerca de Catalunya
instname
Dipòsit Digital de la UB
Universidad de Barcelona
instname
Dipòsit Digital de la UB
Universidad de Barcelona
Se señala la presencia de caliche fósil en el Triásico inferior y el cual es interpretado como caliche inicialmente maduro producido en cortas exposiciones subáreas en condiciones semiáridas. Se deducen das tipos de ambientes de acuerdo con los
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::48f54aa43a309fdf69c1e8d31c947e20
https://hdl.handle.net/2445/32834
https://hdl.handle.net/2445/32834