Zobrazeno 1 - 10
of 69
pro vyhledávání: '"Rubén Díez-Fernández"'
Publikováno v:
Geogaceta, Vol 69 (2021)
La asociación espacial y cinemática entre kink bands en rocas con foliación varisca y cabalgamientos alpinos en el basamento del Sistema Central, permiten deducir que los primeros tienen una edad cenozoica, y no varisca o tardivarisca. Sistemátic
Externí odkaz:
https://doaj.org/article/a7c2b23dc02641e49d360d7b170bb708
Publikováno v:
International Geology Review. :1-14
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bb526f8df315b308c023c91437f6ba33
https://doi.org/10.1080/00206814.2022.2127126
https://doi.org/10.1080/00206814.2022.2127126
Autor:
Esther Rojo-Pérez, Ulf Linnemann, Mandy Hofmann, José M. Fuenlabrada, Johannes Zieger, Javier Fernández-Suárez, Pilar Andonaegui, Sonia Sánchez Martínez, Rubén Díez Fernández, Ricardo Arenas
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
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[EN] In the peri-Gondwanan Ediacaran arc section outcropping in the SW of the Iberian Massif (Mérida region), changes in the subduction angle and subduction rate, variable participation of highly modified mantle sources together with the role of old
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8dc3bee8900b76507047e9d2a8fd615a
https://doi.org/10.1016/j.gr.2022.04.011
https://doi.org/10.1016/j.gr.2022.04.011
Autor:
Rubén Díez Fernández, Irene Novo-Fernández, Diana Moreno-Martín, Ricardo Arenas, Esther Rojo-Pérez, Luis Miguel Martín Parra, Jerónimo Matas
Publikováno v:
Geological Society, London, Special Publications. 542
Exhumation of high-pressure (P) rocks may require a long path and multiple deformation phases. During this journey, late faults and folds can introduce changes to the primary tectonic stacking and lead to misleading conclusions regarding subduction p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b0a41ea21850e443798c2f09a8b454ff
https://doi.org/10.1144/sp542-2022-308
https://doi.org/10.1144/sp542-2022-308
Autor:
Ricardo Arenas, Christian Vérard, Richard Albert, Esther Rojo-Pérez, Sonia Sánchez Martínez, Irene Novo-Fernández, Diana Moreno-Martín, Axel Gerdes, Antonio Garcia-Casco, Rubén Díez Fernández
Publikováno v:
Geological Society, London, Special Publications. 542
The recent discovery of Ediacaran ophiolites in the SW Iberian Massif has made it possible to pinpoint the evolution of the Cadomian basement of Europe. The Calzadilla and Merida ophiolites (gabbroic protoliths dated at c. 600 and 594 Ma, respectivel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ad708116bd4e23e6fe25fc1095639649
https://doi.org/10.1144/sp542-2022-328
https://doi.org/10.1144/sp542-2022-328
Autor:
Esther Rojo-Pérez, Ricardo Arenas, José M. Fuenlabrada, Irene Novo-Fernández, Sonia Sánchez Martínez, Diana Moreno-Martín, Rubén Díez Fernández
Publikováno v:
Geological Society, London, Special Publications. 542
Aspects of the evolution of the Pan-African-Cadomian arc have been recognized in several European massifs. The Ossa-Morena Complex (SW Iberian Massif) is one of the best-preserved sections of this paleo-Gondwana margin. In this domain, recent studies
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e6fe2aaa33ab506fce46c47139cc0fa9
https://doi.org/10.1144/sp542-2022-294
https://doi.org/10.1144/sp542-2022-294
Autor:
Francisco J. Rubio Pascual, Luis M. Martín Parra, Rubén Díez Fernández, Pablo Valverde-Vaquero, Alejandro Díez-Montes, Manuel P. Hacar Rodríguez, Justo Iglesias, Gloria Gallastegui, L. Roberto Rodríguez Fernández, Aratz Beranoaguirre
Publikováno v:
International Geology Review. :1-25
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::59a7db0185846b6c93d95b16dd5992cb
https://doi.org/10.1080/00206814.2022.2073569
https://doi.org/10.1080/00206814.2022.2073569
Publikováno v:
E-Prints Complutense. Archivo Institucional de la UCM
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The Spanish–Portuguese Central System (SPCS) is an Alpine Mountain range with crystalline basement characterised by a two-layer rheological structure. This structure formed after primary (protolith) and secondary (tectonometamorphic) processes duri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::434037eefa7ba47c99f2e07905ddc52a
https://doi.org/10.1029/2022tc007315
https://doi.org/10.1029/2022tc007315
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
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This article is a reply to a comment by Azor et al. (2022), https://doi.org/10.1029/2021TC006982.
[EN] Geological mapping, structural data, and analytical modeling by Díez Fernández et al. (2021), https://doi.org/10.1029/2021tc006791 supported
[EN] Geological mapping, structural data, and analytical modeling by Díez Fernández et al. (2021), https://doi.org/10.1029/2021tc006791 supported
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::89e99a1a1025698ced57ff14d737c86d
http://hdl.handle.net/10261/272445
http://hdl.handle.net/10261/272445
Autor:
Rubén Díez Fernández, José Manuel Fuenlabrada, Ricardo Arenas, Sonia Sánchez Martínez, Esther Rojo-Pérez
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
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[EN] Neoproterozoic and Palaeozoic rocks of the Mérida Massif (SW Iberia) have been grouped into tectonostratigraphic units. Each unit is separated from the rest ones by either crustal-scale thrusts and/or extensional detachments. The lowermost unit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4e8891bc1ebee61aeb6f142fc7ab20db
http://hdl.handle.net/10261/269726
http://hdl.handle.net/10261/269726