Zobrazeno 1 - 10
of 103
pro vyhledávání: '"F. GONZÁLEZ-LODEIRO"'
Autor:
M. VÁZQUEZ, L. ASEBRIY, A. AZDIMOUSA, A. JABALOY, G. BOOTH-REA, L. BARBERO, M. MELLINI, F. GONZÁLEZ-LODEIRO
Publikováno v:
Geologica Acta, Vol 13, Iss 1 (2015)
None
Externí odkaz:
https://doaj.org/article/12c9837d665b403b87390a63892acff7
Autor:
M. VÁZQUEZ, L. ASEBRIY, A. AZIMOUSA, A. JABALOY, G. BOOTH-REA, L. BARBERO, M. MELLINI, F. GONZÁLEZ-LODEIRO
Publikováno v:
Geologica Acta, Vol 11, Iss 3 (2013)
The distribution pattern of diagenetic conditions to very low-grade metamorphism in the eastern Rif has been determined based on a study of clay-mineral assemblages and illite crystallinity of Mesozoic metapelites. Low-grade conditions were reached i
Externí odkaz:
https://doaj.org/article/631ffdf7209d46ec9e9dfa2603f3c8e8
Publikováno v:
Solid Earth, Vol 7, Iss 3, Pp 857-872 (2016)
Different transpressional scenarios have been proposed to relate kinematics and complex deformation patterns. We apply the most suitable of them to the Variscan orogeny in SW Iberia, which is characterized by a number of successive left-lateral trans
Externí odkaz:
https://doaj.org/article/92b82ef6728e4e1cba4183870315fc61
Autor:
I. DeFelipe, P. Ayarza, I. Palomeras, M. Ruiz, J. Andrés, J. Alcalde, D. Martínez Poyatos, F. González Lodeiro, M. Yenes, J. Elez, I. Pérez‐Cáceres, M. Torne, R. Carbonell
Publikováno v:
Tectonics. 41
Intraplate ranges are topographic features that can occur far from plate boundaries, the expected position of orogens as described in the plate tectonics theory. To understand the lithospheric structure of intraplate ranges, we focused on the Spanish
Autor:
Í. Dias da Silva, Aina Margalef, Irene Pérez-Cáceres, J. R. Martínez Catalán, Antonio Azor, D. Martínez Poyatos, Inmaculada Expósito, J. Gómez Barreiro, José Fernando Simancas, Josep Maria Casas, Pilar Clariana, F. González Lodeiro, E. González-Clavijo, Joaquín García-Sansegundo
Publikováno v:
The Geology of Iberia: A Geodynamic Approach ISBN: 9783030105181
The Variscan deformation in the Iberian Massif is related to the large-scale plate tectonic scenario that drove to the destruction of the Rheic and other intervening oceans, to finally form the Pangea Supercontinent. The Northern Iberian Massif struc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ad95d4682eb0df3066888d6f69675f3e
https://doi.org/10.1007/978-3-030-10519-8_10
https://doi.org/10.1007/978-3-030-10519-8_10
Autor:
Irene Pérez-Cáceres, D. Martínez Poyatos, José Fernando Simancas, F. González Lodeiro, Antonio Azor, Inmaculada Expósito
Publikováno v:
Tectonophysics. 666:281-284
A vast Variscan nappe spreading from the Allochthonous Complexes of NW Iberia to the Ossa-Morena Zone in SW Iberia has been proposed by Diez Fernandez and Arenas (2015) , based on the correlation of different outcrops of high-pressure and MORB-type r
Autor:
Jacques Bourgois, Guillermo Booth-Rea, Ali Azdimousa, Antonio Jabaloy-Sánchez, L. Asebriy, F. González-Lodeiro, José Miguel Martínez-Martínez, Philippe Münch, M. Vázquez-Vílchez
Publikováno v:
Journal of African Earth Sciences
Journal of African Earth Sciences, Elsevier, 2018, 150, pp.657-672. ⟨10.1016/j.jafrearsci.2018.09.018⟩
Digital.CSIC. Repositorio Institucional del CSIC
instname
Journal of African Earth Sciences, Elsevier, 2018, 150, pp.657-672. ⟨10.1016/j.jafrearsci.2018.09.018⟩
Digital.CSIC. Repositorio Institucional del CSIC
instname
The Cap des Trois Fourches (Eastern Rif, northern Morocco) metamorphic basement exposes two major tectonic units, namely the Taïdant unit underthrusting the overlying Tarjât tectonic unit. The Tarjât tectonic unit is composed of metamorphic rock o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d2da760c6daa2ec7e229ace6c1800dd1
https://hal.archives-ouvertes.fr/hal-01884964
https://hal.archives-ouvertes.fr/hal-01884964
Publikováno v:
International Journal of Earth Sciences. 104:1739-1757
New SHRIMP U–Pb ages of detrital zircons from Neoproterozoic low-grade metasandstones of the Schist–Graywacke Complex (Central Iberian Zone, Iberian Massif) sampled just below and above the intra-Alcudian unconformity at two selected locations co
Publikováno v:
Estudios Geologicos, Vol 48, Iss 3-4, Pp 163-164 (1992)
No disponible
Externí odkaz:
https://doaj.org/article/a3f0f99971e646a1a8569f0ebcae7957
Autor:
Ramón Carbonell, José Fernando Simancas, F. González Lodeiro, Antonio Azor, Andrés Pérez-Estaún, Puy Ayarza, D. Martínez Poyatos
Publikováno v:
Tectonics. 32:417-432
[1] A crustal geotraverse through the Iberian Variscides is presented by integrating the available geological and seismic profiling data. Different modes of orogenic shortening are identified, with varying degrees of coupling between upper and lower