Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Francisco J. Rubio Pascual"'
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:
Geoscience Frontiers, Vol 10, Iss 2, Pp 651-669 (2019)
This contribution discusses about the rheological, kinematic and dynamic frameworks necessary to produce recumbent and upright folds from syn-orogenic granitic massifs that were formed during an early stage of magma genesis related to the onset of a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0c1e959b1aa6483458ade366ec59f114
http://www.sciencedirect.com/science/article/pii/S1674987118300860
http://www.sciencedirect.com/science/article/pii/S1674987118300860
Autor:
Rubén Díez Fernández, Nemesio Heredia, P. Valverde-Vaquero, Gloria Gallastegui, Justo Iglesias, Manuel P. Hacar Rodríguez, L. Roberto Rodríguez Fernández, Francisco J. Rubio Pascual, Alejandro Díez Montes, Luis Miguel Martín Parra
A stacking of nappes forms the Parautochthonous Domain located beneath the Allochthonous Complexes of the NW Iberian Massif. Lower Paleozoic metasedimentary and felsic metavolcanic rocks, including some riebeckite gneiss, form the uppermost nappe of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aecce9de416c2998d82c8919f07b6a1c
https://doi.org/10.5194/se-2020-25
https://doi.org/10.5194/se-2020-25
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
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This contribution provides a case example on the generation of large-scale recumbent folds in syn-orogenic granitoids. We analyze the progressive reworking of extension-related structures into later ones after a period of crustal thickening. The Padr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::237da1a56469cf7d58deaf1378b22650
https://doi.org/10.1016/j.tecto.2017.03.010
https://doi.org/10.1016/j.tecto.2017.03.010
Autor:
Rubén Díez Fernández, Jerónimo Matas, Ricardo Arenas, Sonia Sánchez-Martínez, Richard Albert, Luis-Miguel Martín Parra, M. Francisco Pereira, Francisco-J. Rubio Pascual
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
An integrated interpretation of the late Paleozoic structural and geochronological record of the Iberian Massif is presented and discussed under the perspective of a Gondwana-Laurussia collision giving way to the Variscan orogen. Compressional and ex
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c84917ec5bc5c3fd8b43cd38a3e5daaa
https://doi.org/10.1016/j.earscirev.2016.08.002
https://doi.org/10.1016/j.earscirev.2016.08.002
Autor:
Rubén Díez Fernández, Sonia Sánchez Martínez, José Manuel Fuenlabrada, Alicia López Carmona, Javier Fernández-Suárez, Pilar Andonaegui, Jacobo Abati, Ricardo Arenas, Richard Albert, Axel Gerdes, Pablo González Cuadra, Francisco J. Rubio Pascual
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
NW Iberia includes a rather complete section of a Variscan suture, where different terranes with continental or oceanic affinities appear with clear structural relationships. Three groups of terranes, namely Upper, Ophiolitic and Basal units and a fr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::48e877ea9b5b2f7cfd81088b2ffd420e
https://doi.org/10.1016/j.earscirev.2016.08.010
https://doi.org/10.1016/j.earscirev.2016.08.010
Autor:
Alberto Jiménez-Díaz, Rubén Díez Fernández, Javier Fernández-Suárez, Luis Miguel Martín Parra, José Manuel Fuenlabrada, Ricardo Arenas, Pilar Montero, Richard Albert, M. Francisco Pereira, Pilar Andonaegui, Francisco J. Rubio Pascual, Sonia Sánchez Martínez, Jerónimo Matas
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Agência para a Sociedade do Conhecimento (UMIC)-FCT-Sociedade da Informação
instacron:RCAAP
instname
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Agência para a Sociedade do Conhecimento (UMIC)-FCT-Sociedade da Informação
instacron:RCAAP
In the Ossa Morena Domain of SW Iberia, the Calzadilla Ophiolite is formed by an ensemble of ultramafic and mafic rocks that seem to represent a fragment of an oceanic Moho transition zone. The ophiolite consists of a main sheet with a minimum thickn
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5baeeb5867b5fd73193edd0847cb1c07
http://hdl.handle.net/10261/186586
http://hdl.handle.net/10261/186586
Autor:
Francisco J. Rubio Pascual, Emilio González Clavijo, Juan Gómez Barreiro, Ícaro Dias da Silva, Alejandro Díez Montes, Ricardo Arenas, José R. Martínez Catalán, James E. Alcock, Rubén Díez Fernández
Publikováno v:
Tectonophysics. 657:21-37
A model for the P–T–t evolution of NW and Central Iberia is presented to better understand its metamorphic evolution from initial Barrovian stage through HT–LP conditions. The model is constrained by the well-known succession of structural even
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9ff272e6c0cec1a71651675107dc1b59
https://doi.org/10.1016/j.tecto.2015.05.022
https://doi.org/10.1016/j.tecto.2015.05.022
Autor:
Emilio González Clavijo, Juan Gómez Barreiro, José R. Martínez Catalán, Francisco J. Rubio Pascual, James E. Alcock, Alejandro Díez Montes, Ícaro Dias da Silva, Rubén Díez Fernández, Puy Ayarza
Publikováno v:
Geological Society, London, Special Publications. 405:225-247
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::61c3cb7fffa776b4bc412887bd0ca712
https://doi.org/10.1144/sp405.1
https://doi.org/10.1144/sp405.1
Publikováno v:
Tectonophysics. 592:187-199
Several units exposed in the boundary area of the Ossa Morena Zone (OMZ) and the South Portuguese Zone (SPZ) preserve petrographic and thermobarometric evidence for an early metamorphic episode (M1), developed under a high- P , low to intermediate- T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4cae58f15b1fee78ae1e0cdec31007be
https://doi.org/10.1016/j.tecto.2013.02.022
https://doi.org/10.1016/j.tecto.2013.02.022