14 citations as recorded by crossref.

1. Characterizing the Source of the Eastern Galicia Magnetic Anomaly (NW Spain): The Role of Extension in the Origin of Magnetization at the Central Iberian Arc P. Ayarza et al. 10.1029/2020TC006120
2. The orogenic bridge theory: towards a predictive tool for past and future plate tectonics J. Koehl & G. Foulger 10.12688/openreseurope.17238.1
3. Neoproterozoic–paleozoic detrital sources in the Variscan foreland of northern Iberia: primary v. recycled sediments G. Gutiérrez-Alonso et al. 10.1144/SP503-2020-21
4. Evolution of the Alpine orogenic belts in the Western Mediterranean region as resolved by the kinematics of the Europe-Africa diffuse plate boundary P. Angrand et al. 10.1051/bsgf/2021031
5. Oroclinal arcs of the Variscan Belt: a consequence of transpression during the consolidation of Pangaea J. Martínez Catalán et al. 10.1144/jgs2024-007
6. Orogenic bridge theory: towards a predictive tool for past and future plate tectonics J. Koehl & G. Foulger 10.12688/openreseurope.17238.2
7. From source to surface: clues from garnet-bearing Carboniferous silicic volcanic rocks, Iberian Pyrite Belt, Portugal A. Cravinho et al. 10.1007/s00410-024-02106-3
8. Avalonia, get bent! – Paleomagnetism from SW Iberia confirms the Greater Cantabrian Orocline B. Leite Mendes et al. 10.1016/j.gsf.2020.07.013
9. From supercontinent to superplate: Late Paleozoic Pangea's inner deformation suggests it was a short-lived superplate D. Pastor-Galán 10.1016/j.earscirev.2022.103918
10. Matching mid-to-latest Carboniferous pole path segments for eastern Australia and northern Armorica indicate a late Carboniferous Pangea-B configuration and a mid Carboniferous inertial interchange true polar wander event C. Klootwijk 10.1016/j.earscirev.2023.104521
11. Reconstructing the pre-Variscan puzzle of Cambro-Ordovician basement rocks in the southwestern European margin of Gondwana J. Álvaro et al. 10.1144/SP503-2020-89
12. Is the Ibero-Armorican Arc primary or secondary? An analysis of the contraction required to form it by rotation around a vertical axis J. Casas et al. 10.1144/jgs2021-065
13. Late- to post-Variscan tectonics and the kinematic relationship with W–Sn vein-type mineralization: evidence from Late Carboniferous intramontane basins (Porto–Sátão syncline, Variscan Iberian belt) D. Jacques et al. 10.1144/jgs2020-223
14. Paleomagnetism in the Cambrian Urda-Los Navalucillos Limestone (Montes de Toledo, Spain): Implications for late-Variscan kinematics and oroclinal bending in the Central Iberian Zone M. Durán Oreja et al. 10.1016/j.tecto.2023.229781