Articles | Volume 11, issue 4
https://doi.org/10.5194/se-11-1291-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/se-11-1291-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Chronostratigraphic framework and provenance of the Ossa-Morena Zone Carboniferous basins (southwest Iberia)
Manuel Francisco Pereira
CORRESPONDING AUTHOR
Instituto de Ciências da Terra, Departamento de Geociências, ECT, Universidade de Évora, Apt. 94, Évora, 7002-554, Portugal
Cristina Gama
Instituto de Ciências da Terra, Departamento de Geociências, ECT, Universidade de Évora, Apt. 94, Évora, 7002-554, Portugal
Ícaro Dias da Silva
Instituto Dom Luiz, Faculdade de Ciências da Universidade de Lisboa, Campo Grande, Lisbon, 1749-016, Portugal
José Brandão Silva
Instituto Dom Luiz, Departamento de Geologia, Faculdade de Ciências da Universidade de Lisboa, Campo Grande, Lisbon, 1749-016, Portugal
Mandy Hofmann
Senckenberg Naturhistorische Sammlungen Dresden, Museum für Mineralogie und Geologie, Dresden, Germany
Ulf Linnemann
Senckenberg Naturhistorische Sammlungen Dresden, Museum für Mineralogie und Geologie, Dresden, Germany
Andreas Gärtner
Senckenberg Naturhistorische Sammlungen Dresden, Museum für Mineralogie und Geologie, Dresden, Germany
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Cited
12 citations as recorded by crossref.
- Visean high-K mafic–intermediate plutonic rocks of the Ossa–Morena Zone (SW Iberia): implications for regional extensional tectonics M. Pereira et al. 10.1144/SP531-2022-118
- A tectonic carpet of Variscan flysch at the base of a rootless accretionary prism in northwestern Iberia: U–Pb zircon age constrains from sediments and volcanic olistoliths E. González Clavijo et al. 10.5194/se-12-835-2021
- Transcurrent displacement of the Cadomian magmatic arc A. Azor et al. 10.1016/j.precamres.2021.106251
- The Carboniferous shoshonitic (s.l.) gabbro–monzonitic stocks of Veiros and Vale de Maceira, Ossa-Morena Zone (SW Iberian Massif): Evidence for diverse subduction-related lithospheric metasomatism J. Lains Amaral et al. 10.1016/j.chemer.2022.125917
- The paleotectonic evolution of the western Mediterranean: provenance insights from the internal Betics, southern Spain E. Poulaki & D. Stockli 10.3389/feart.2022.929502
- U-Pb ages and Hf isotopic composition of detrital zircon in western Algarve Triassic sandstone (SW Iberia): Implications for crustal evolution, provenance, and paleogeography M. Pereira & C. Gama 10.1016/j.lithos.2024.107871
- Using U-Pb detrital zircon systematics to constrain the architecture and provenance of the Ronda peridotites’ crustal hanging wall, S Spain A. Azor et al. 10.1016/j.gr.2024.06.012
- Enhancing, Disseminating, and Preserving the Rio Almansor Migmatites Geosite (Montemor-o-Novo, SW Portugal) M. Pereira et al. 10.1007/s12371-025-01129-x
- Changing Carboniferous Arc Magmatism in the Ossa-Morena Zone (Southwest Iberia): Implications for the Variscan Belt M. Pereira et al. 10.3390/min12050597
- Variscan intracrustal recycling by melting of Carboniferous arc-like igneous protoliths (Évora Massif, Iberian Variscan belt) C. Rodríguez et al. 10.1130/B36111.1
- U-Pb geochronology of detrital and igneous zircon grains from the Águilas Arc in the Internal Betics (SE Spain): Implications for Carboniferous-Permian paleogeography of Pangea A. Jabaloy-Sánchez et al. 10.1016/j.gr.2020.10.013
- The influence of synorogenic extension on the crustal architecture of North Gondwana during the assembly of Pangaea (Ossa–Morena Zone, SW Iberia) Í. Dias da Silva et al. 10.1144/SP542-2023-9
12 citations as recorded by crossref.
- Visean high-K mafic–intermediate plutonic rocks of the Ossa–Morena Zone (SW Iberia): implications for regional extensional tectonics M. Pereira et al. 10.1144/SP531-2022-118
- A tectonic carpet of Variscan flysch at the base of a rootless accretionary prism in northwestern Iberia: U–Pb zircon age constrains from sediments and volcanic olistoliths E. González Clavijo et al. 10.5194/se-12-835-2021
- Transcurrent displacement of the Cadomian magmatic arc A. Azor et al. 10.1016/j.precamres.2021.106251
- The Carboniferous shoshonitic (s.l.) gabbro–monzonitic stocks of Veiros and Vale de Maceira, Ossa-Morena Zone (SW Iberian Massif): Evidence for diverse subduction-related lithospheric metasomatism J. Lains Amaral et al. 10.1016/j.chemer.2022.125917
- The paleotectonic evolution of the western Mediterranean: provenance insights from the internal Betics, southern Spain E. Poulaki & D. Stockli 10.3389/feart.2022.929502
- U-Pb ages and Hf isotopic composition of detrital zircon in western Algarve Triassic sandstone (SW Iberia): Implications for crustal evolution, provenance, and paleogeography M. Pereira & C. Gama 10.1016/j.lithos.2024.107871
- Using U-Pb detrital zircon systematics to constrain the architecture and provenance of the Ronda peridotites’ crustal hanging wall, S Spain A. Azor et al. 10.1016/j.gr.2024.06.012
- Enhancing, Disseminating, and Preserving the Rio Almansor Migmatites Geosite (Montemor-o-Novo, SW Portugal) M. Pereira et al. 10.1007/s12371-025-01129-x
- Changing Carboniferous Arc Magmatism in the Ossa-Morena Zone (Southwest Iberia): Implications for the Variscan Belt M. Pereira et al. 10.3390/min12050597
- Variscan intracrustal recycling by melting of Carboniferous arc-like igneous protoliths (Évora Massif, Iberian Variscan belt) C. Rodríguez et al. 10.1130/B36111.1
- U-Pb geochronology of detrital and igneous zircon grains from the Águilas Arc in the Internal Betics (SE Spain): Implications for Carboniferous-Permian paleogeography of Pangea A. Jabaloy-Sánchez et al. 10.1016/j.gr.2020.10.013
- The influence of synorogenic extension on the crustal architecture of North Gondwana during the assembly of Pangaea (Ossa–Morena Zone, SW Iberia) Í. Dias da Silva et al. 10.1144/SP542-2023-9
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Short summary
A chronostratigraphic study was conducted on Carboniferous rocks of SW Iberia. Terrigenous strata with a maximum depositional age of ca. 303 Ma unconformably overlie marine deposits and volcanic rocks dated at ca. 335–331 Ma. Lying below this unconformity, the marine deposits are intruded and overlain by a ca. 317 Ma porphyry. Detrital zircon populations from marine deposits indicate derivation from Laurussian terranes, while the terrestrial rocks are related to Laurussia and Gondwana sources.
A chronostratigraphic study was conducted on Carboniferous rocks of SW Iberia. Terrigenous...