| Constraints imposed by rift inheritance on the compressional reactivation of a hyperextended margin: Mapping rift domains in the North Iberian margin and in the Cantabrian … P Cadenas, G Fernández‐Viejo, JA Pulgar, J Tugend, G Manatschal, ... Tectonics 37 (3), 758-785, 2018 | 63 | 2018 |
| Permian-Triassic rifting stage J López-Gómez, J Alonso-Azcárate, A Arche, J Arribas, ... The Geology of Iberia: A Geodynamic Approach: Volume 3: The Alpine Cycle, 29-112, 2019 | 60 | 2019 |
| New lithostratigraphy for the Cantabrian Mountains: A common tectono-stratigraphic evolution for the onset of the Alpine cycle in the W Pyrenean realm, N Spain J López-Gómez, F Martín-González, N Heredia, R de La Horra, ... Earth-Science Reviews 188, 249-271, 2019 | 48 | 2019 |
| The Asturian Basin within the North Iberian margin (Bay of Biscay): seismic characterisation of its geometry and its Mesozoic and Cenozoic cover P Cadenas, G Fernández‐Viejo Basin Research 29 (4), 521-541, 2017 | 36 | 2017 |
| The role of inheritance in forming rifts and rifted margins and building collisional orogens: a Biscay-Pyrenean perspective G Manatschal, P Chenin, R Lescoutre, J Miró, P Cadenas, N Saspiturry, ... BSGF-Earth Sciences Bulletin 192 (1), 55, 2021 | 33 | 2021 |
| How much confidence can be conferred on tectonic maps of continental shelves? The Cantabrian-Fault case FV Gabriela, LF Carlos, DCM José, C Patricia Scientific Reports 4 (1), 3661, 2014 | 29 | 2014 |
| Unravelling the architecture and evolution of the inverted multi-stage North Iberian-Bay of Biscay rift P Cadenas, G Manatschal, G Fernández-Viejo Gondwana Research 88, 67-87, 2020 | 28 | 2020 |
| IMAGinING RIFTING G Peron-Pinvidic, G Manatschal, T Alves, TB Andersen, ... Workshop Participants, 1-8, 2019 | 21 | 2019 |
| Reactivation of a hyperextended rift system: The Basque–Cantabrian Pyrenees case J Miró, G Manatschal, P Cadenas, JA Muñoz Basin Research 33 (6), 3077-3101, 2021 | 19 | 2021 |
| Investigating the plate kinematics of the Bay of Biscay using deformable plate tectonic models MT King, JK Welford, P Cadenas, J Tugend Tectonics 40 (7), e2020TC006467, 2021 | 17 | 2021 |
| A kinematic reconstruction of Iberia using intracontinental strike‐slip corridors G Frasca, G Manatschal, P Cadenas, J Miró, R Lescoutre Terra Nova 33 (6), 573-581, 2021 | 14 | 2021 |
| The unevenness of the north Iberian crustal root, a snapshot of an elusive stage in margin reactivation G Fernández-Viejo, P Cadenas, J Acevedo, S Llana-Fúnez Geology 49 (12), 1426-1430, 2021 | 6 | 2021 |
| The role of extensional detachment systems in thinning the crust and exhuming granulites: analogies between the offshore Le Danois High and the onshore Labourd Massif in the … P Cadenas, R Lescoutre, G Manatschal, G Fernández-Viejo Bulletin de la Société géologique de France 192 (1), 2021 | 6 | 2021 |
| Structure and tectonic evolution of the NW Sulu Sea Basin (SE Asia) P Cadenas, CR Ranero Journal of Geophysical Research: Solid Earth 129 (3), e2022JB026180, 2024 | 3 | 2024 |
| Margin segmentation during polyphase rifting in the southern Bay of Biscay P Cadenas, G Manatschal, G Fernández-Viejo, JK Welford Atl. Geol. 54, 409-470, 2018 | 3 | 2018 |
| Seismic interpretation of the Cantabrian platform around “Le Danois Bank”, Bay of Biscay P Cadenas, C López-Fernández, J Gallastegui, G Fernández-Viejo Geotemas 13, 1702-1705, 2012 | 3 | 2012 |
| Subduction initiation, propagation and progression recorded along the Sulu and Celebes seas (SE Asia) PC Martínez, CR Ranero EGU24, 2024 | | 2024 |
| (D)rifting in the 21st century: Key processes, natural hazards and geo-resources F Zwaan, T Alves, P Cadenas, M Gouiza, J Phethean, S Brune, A Glerum EGUsphere 2023, 1-58, 2023 | | 2023 |
| Offshore seismicity clusters in the West Iberian Margin illustrated by 2 decades of events G Fernández-Viejo, C López-Fernández, P Cadenas Solid Earth 14 (10), 1083-1101, 2023 | | 2023 |
| Offshore seismicity clusters in the West iberian Margin illustrated by two decades of events G Fernandez-Viejo, C Lopez-Fernandez, P Cadenas EGUsphere 2023, 1-29, 2023 | | 2023 |
