| The South Shetland Islands, Antarctica: Lithostratigraphy and geological map | Frontiers in earth science |  | | 2023 | 264 | 153 |
|
| Cretaceous magmatism in the Antarctic Peninsula and its tectonic implications | Journal of the Geological Society |  | | 2022 | 234 | 0 |
|
| Data on the arc magmatism developed in the Antarctic Peninsula and Patagonia during the Late Triassic–Jurassic: A compilation of new and previous geochronology, geochemistry and isotopic tracing results | Data in Brief |  | | 2021 | 256 | 250 |
|
| A revised interpretation of the Chon Aike magmatic province: Active margin origin and implications for the opening of the Weddell Sea | Lithos |  | | 2021 | 230 | 244 |
|
| The Gondwanan margin in West Antarctica: Insights from Late Triassic magmatism of the Antarctic Peninsula | Gondwana Research |  | | 2020 | 413 | 2 |
|
| The Triassic–Cretaceous Tectonomagmatic History of the Antarctic Peninsula constrained by Geochronology, Thermochronology and Isotope Geochemistry | |  | | 2020 | 756 | 594 |
|
| The Byers Basin: Jurassic-Cretaceous tectonic and depositional evolution of the forearc deposits of the South Shetland Islands and its implications for the northern Antarctic Peninsula | International Geology Review |  | | 2019 | 423 | 0 |
|
| Geochronology and geochemistry of the northern Scotia Sea: A revised interpretation of the North and West Scotia ridge junction | Earth and Planetary Science Letters |  | | 2019 | 775 | 428 |
|
| Genetic Structure and Gene Flow of Moss Sanionia uncinata (Hedw.) Loeske in Maritime Antarctica and Southern-Patagonia | Frontiers in Ecology and Evolution |  | | 2018 | 540 | 374 |
|
| Provenance, transport and diagenesis of sediment in polar areas: a case study in Profound Lake, King George Island, Antarctica | Polar Research |  | | 2018 | 485 | 318 |
|
| Very low-grade secondary minerals as indicators of palaeo-hydrothermal systems in the Upper Cretaceous volcanic succession of Hannah Point, Livingston Island, Antarctica | Applied Clay Science |  | | 2016 | 456 | 0 |
|