Articles | Volume 7, issue 3
https://doi.org/10.5194/se-7-857-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-7-857-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
30 May 2016
Research article |
| 30 May 2016
Oblique collision and deformation partitioning in the SW Iberian Variscides
Departamento de Geodinámica, Facultad de Ciencias, Universidad
de Granada, Campus de Fuentenueva s/n, 18071 Granada, Spain
José Fernando Simancas
Departamento de Geodinámica, Facultad de Ciencias, Universidad
de Granada, Campus de Fuentenueva s/n, 18071 Granada, Spain
David Martínez Poyatos
Departamento de Geodinámica, Facultad de Ciencias, Universidad
de Granada, Campus de Fuentenueva s/n, 18071 Granada, Spain
Antonio Azor
Departamento de Geodinámica, Facultad de Ciencias, Universidad
de Granada, Campus de Fuentenueva s/n, 18071 Granada, Spain
Francisco González Lodeiro
Departamento de Geodinámica, Facultad de Ciencias, Universidad
de Granada, Campus de Fuentenueva s/n, 18071 Granada, Spain
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Cited
17 citations as recorded by crossref.
- Reassessing the lithosphere: SeisDARE, an open-access seismic data repository I. DeFelipe et al. https://doi.org/10.5194/essd-13-1053-2021
- Pre-Variscan (Lower Devonian) deformation of the Silurian magmatic arc of the East Odenwald (Mid-German Crystalline Zone, Variscides) H. Meinaß et al. https://doi.org/10.1127/zdgg/2022/0328
- Building and Collapse of the Cadomian Orogen: A Plate‐Scale Model Based on Structural Data From the SW Iberian Massif D. Moreno‐Martín et al. https://doi.org/10.1029/2023TC007990
- The enigmatic curvature of Central Iberia and its puzzling kinematics D. Pastor-Galán et al. https://doi.org/10.5194/se-11-1247-2020
- Tectonic Evolution of the Eastern Moroccan Meseta: From Late Devonian Forearc Sedimentation to Early Carboniferous Collision of an Avalonian Promontory C. Accotto et al. https://doi.org/10.1029/2019TC005976
- The Mid-Variscan Allochthon: Keys from correlation, partial retrodeformation and plate-tectonic reconstruction to unlock the geometry of a non-cylindrical belt J. Martínez Catalán et al. https://doi.org/10.1016/j.earscirev.2021.103700
- Deciphering the metamorphic evolution of the Pulo do Lobo metasedimentary domain (SW Iberian Variscides) I. Pérez-Cáceres et al. https://doi.org/10.5194/se-11-469-2020
- Evolution of the Iberian Massif as deduced from its crustal thickness and geometry of a mid-crustal (Conrad) discontinuity P. Ayarza et al. https://doi.org/10.5194/se-12-1515-2021
- Avalonia, get bent! – Paleomagnetism from SW Iberia confirms the Greater Cantabrian Orocline B. Leite Mendes et al. https://doi.org/10.1016/j.gsf.2020.07.013
- Transcurrent displacement of the Cadomian magmatic arc A. Azor et al. https://doi.org/10.1016/j.precamres.2021.106251
- Chronostratigraphic framework and provenance of the Ossa-Morena Zone Carboniferous basins (southwest Iberia) M. Pereira et al. https://doi.org/10.5194/se-11-1291-2020
- Variscan intracrustal recycling by melting of Carboniferous arc-like igneous protoliths (Évora Massif, Iberian Variscan belt) C. Rodríguez et al. https://doi.org/10.1130/B36111.1
- From a bipartite Gondwanan shelf to an arcuate Variscan belt: The early Paleozoic evolution of northern Peri-Gondwana T. Stephan et al. https://doi.org/10.1016/j.earscirev.2019.03.012
- The evolution of the subcontinental mantle beneath the Central Iberian Zone: Geochemical tracking of its mafic magmatism from the Neoproterozoic to the Cenozoic C. Villaseca et al. https://doi.org/10.1016/j.earscirev.2022.103997
- Coseismic Slip Deficit of the 2017 Mw 6.5 Ormoc Earthquake That Occurred Along a Creeping Segment and Geothermal Field of the Philippine Fault Y. Yang et al. https://doi.org/10.1002/2017GL076417
- On the Rootless Nature of a Devonian Suture in SW Iberia (Ossa‐Morena Complex, Variscan Orogen): Geometry and Kinematics of the Azuaga Fault R. Fernández et al. https://doi.org/10.1029/2021TC006791
- Ediacaran Obduction of a Fore‐Arc Ophiolite in SW Iberia: A Turning Point in the Evolving Geodynamic Setting of Peri‐Gondwana R. Díez Fernández et al. https://doi.org/10.1029/2018TC005224
17 citations as recorded by crossref.
- Reassessing the lithosphere: SeisDARE, an open-access seismic data repository I. DeFelipe et al. https://doi.org/10.5194/essd-13-1053-2021
- Pre-Variscan (Lower Devonian) deformation of the Silurian magmatic arc of the East Odenwald (Mid-German Crystalline Zone, Variscides) H. Meinaß et al. https://doi.org/10.1127/zdgg/2022/0328
- Building and Collapse of the Cadomian Orogen: A Plate‐Scale Model Based on Structural Data From the SW Iberian Massif D. Moreno‐Martín et al. https://doi.org/10.1029/2023TC007990
- The enigmatic curvature of Central Iberia and its puzzling kinematics D. Pastor-Galán et al. https://doi.org/10.5194/se-11-1247-2020
- Tectonic Evolution of the Eastern Moroccan Meseta: From Late Devonian Forearc Sedimentation to Early Carboniferous Collision of an Avalonian Promontory C. Accotto et al. https://doi.org/10.1029/2019TC005976
- The Mid-Variscan Allochthon: Keys from correlation, partial retrodeformation and plate-tectonic reconstruction to unlock the geometry of a non-cylindrical belt J. Martínez Catalán et al. https://doi.org/10.1016/j.earscirev.2021.103700
- Deciphering the metamorphic evolution of the Pulo do Lobo metasedimentary domain (SW Iberian Variscides) I. Pérez-Cáceres et al. https://doi.org/10.5194/se-11-469-2020
- Evolution of the Iberian Massif as deduced from its crustal thickness and geometry of a mid-crustal (Conrad) discontinuity P. Ayarza et al. https://doi.org/10.5194/se-12-1515-2021
- Avalonia, get bent! – Paleomagnetism from SW Iberia confirms the Greater Cantabrian Orocline B. Leite Mendes et al. https://doi.org/10.1016/j.gsf.2020.07.013
- Transcurrent displacement of the Cadomian magmatic arc A. Azor et al. https://doi.org/10.1016/j.precamres.2021.106251
- Chronostratigraphic framework and provenance of the Ossa-Morena Zone Carboniferous basins (southwest Iberia) M. Pereira et al. https://doi.org/10.5194/se-11-1291-2020
- Variscan intracrustal recycling by melting of Carboniferous arc-like igneous protoliths (Évora Massif, Iberian Variscan belt) C. Rodríguez et al. https://doi.org/10.1130/B36111.1
- From a bipartite Gondwanan shelf to an arcuate Variscan belt: The early Paleozoic evolution of northern Peri-Gondwana T. Stephan et al. https://doi.org/10.1016/j.earscirev.2019.03.012
- The evolution of the subcontinental mantle beneath the Central Iberian Zone: Geochemical tracking of its mafic magmatism from the Neoproterozoic to the Cenozoic C. Villaseca et al. https://doi.org/10.1016/j.earscirev.2022.103997
- Coseismic Slip Deficit of the 2017 Mw 6.5 Ormoc Earthquake That Occurred Along a Creeping Segment and Geothermal Field of the Philippine Fault Y. Yang et al. https://doi.org/10.1002/2017GL076417
- On the Rootless Nature of a Devonian Suture in SW Iberia (Ossa‐Morena Complex, Variscan Orogen): Geometry and Kinematics of the Azuaga Fault R. Fernández et al. https://doi.org/10.1029/2021TC006791
- Ediacaran Obduction of a Fore‐Arc Ophiolite in SW Iberia: A Turning Point in the Evolving Geodynamic Setting of Peri‐Gondwana R. Díez Fernández et al. https://doi.org/10.1029/2018TC005224
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