| The 2014–15 eruption and the short-term geochemical evolution of the Fogo volcano (Cape Verde): Evidence for small-scale mantle heterogeneity |
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| 40 Ar/ 39 Ar ages and petrogenesis of the West Iberian Margin onshore magmatism at the Jurassic–Cretaceous transition: Geodynamic implications and assessment of open-system processes involving saline materials |
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| The 9th of July 1998 Faial Island (Azores, North Atlantic) seismic sequence |
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| Assessing landslide movements in volcanic islands using near-shore marine geophysical data: south Pico island, Azores |
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| Chapter 3 Active tectonics in the central and eastern Azores islands along the Eurasia–Nubia boundary: a review |
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| Chapter 6 Volcano-tectonic structures of São Miguel Island, Azores |
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| Condor seamount (Azores, NE Atlantic): A morpho-tectonic interpretation |
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| Constraints on the structure of Maio Island (Cape Verde) by a three-dimensional gravity model: imaging partially exhumed magma chambers |
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| Crustal seismic velocity structure near Faial and Pico Islands (AZORES), from local earthquake tomography |
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| Depositional processes on oceanic island shelves - Evidence from storm-generated Neogene deposits from the mid-North Atlantic |
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| Diverse bioerosion structures in lower Pliocene deposits from a volcanic oceanic island: Baía de Nossa Senhora section, Santa Maria Island, Azores (central North Atlantic) |
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| Emergence and evolution of Santa Maria Island (Azores)—The conundrum of uplifted islands revisited |
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| The emergence of volcanic oceanic islands on a slow-moving plate: The example of Madeira Island, NE Atlantic |
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| Environmental Implication of Subaqueous Lava Flows from A Continental Large Igneous Province: Examples from the Moroccan Central Atlantic Magmatic Province |
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| Extrusive carbonatite outcrops – A source of chemical elements imbalance in topsoils of oceanic volcanic islands |
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| Genesis and morphological evolution of coastal talus-platforms (fajãs) with lagoons: The case study of the newly-formed Fajã dos Milagres (Corvo Island, Azores) |
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| Geochemical evidence for melting of carbonated peridotite on Santa Maria Island, Azores |
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| Geochemical temporal evolution of Brava Island magmatism: Constraints on the variability of Cape Verde mantle sources and on carbonatite–silicate magma link |
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| Geodynamic models for the Azores triple junction: A contribution from tectonics |
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| A geological record of multiple Pleistocene tsunami inundations in an oceanic island: The case of Maio, Cape Verde |
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| Gravitational, erosional and depositional processes on volcanic ocean islands: Insights from the submarine morphology of Madeira Archipelago |
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| Hazard potential of volcanic flank collapses raised by new megatsunami evidence |
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| Incorporating Descriptive Metadata into Seismic Source Zone Models for Seismic-Hazard Assessment: A Case Study of the Azores-West Iberian Region |
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| The insular shelves of the Faial-Pico Ridge |
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| Intraplate seismicity across the Cape Verde swell: A contribution from a temporary seismic network |
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| Inventory and review of the Mio–Pleistocene São Jorge flora (Madeira Island, Portugal): palaeoecological and biogeographical implications |
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| The Jurassic–Cretaceous basaltic magmatism of the Oued El-Abid syncline (High Atlas, Morocco): Physical volcanology, geochemistry and geodynamic implications |
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| Large-scale active slump of the southeastern flank of Pico Island, Azores: COMMENT |
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| Mega-tsunami conglomerates and flank collapses of ocean island volcanoes |
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| Morpho-tectonic analysis of the Azores Volcanic Plateau from a new bathymetric compilation of the area |
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| Morphology, internal architecture and emplacement mechanisms of lava flows from the Central Atlantic Magmatic Province (CAMP) of Argana Basin (Morocco) |
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| The morphology of insular shelves as a key for understanding the geological evolution of volcanic islands: Insights from Terceira Island (Azores) |
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| Palaeoecology, taphonomy, and preservation of a lower Pliocene shell bed (coquina) from a volcanic oceanic island (Santa Maria Island, Azores) |
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| Present-day deformation in São Jorge Island, Azores, from episodic GPS measurements (2001–2011) |
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| Primary and secondary processes constraining the noble gas isotopic signatures of carbonatites and silicate rocks from Brava Island: evidence for a lower mantle origin of the Cape Verde plume |
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| Quaternary extrusive calciocarbonatite volcanism on Brava Island (Cape Verde): A nephelinite-carbonatite immiscibility product |
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| The Quaternary plant fossil record from the volcanic Azores Archipelago (Portugal, North Atlantic Ocean): a review |
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| Rift-related magmatism of the Central Atlantic magmatic province in Algarve, Southern Portugal |
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| Silicic, high- to extremely high-grade ignimbrites and associated deposits from the Paraná Magmatic Province, southern Brazil |
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| Tracing insular woodiness in giant <i>Daucus</i> (s.l.) fruit fossils from the Early Pleistocene of Madeira Island (Portugal) |
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| Vertical land motion and sea level change in Macaronesia |
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| Volcano-stratigraphic and structural evolution of Brava Island (Cape Verde) based on 40Ar/39Ar, U–Th and field constraints |
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| Volcano-tectonic evolution of a linear volcanic ridge (Pico-Faial Ridge, Azores Triple Junction) assessed by paleomagnetic studies |
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| Water prospection in volcanic islands by Time Domain Electromagnetic (TDEM) surveying: The case study of the islands of Fogo and Santo Antão in Cape Verde |
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