Multi-Temporal UAV Data and object-based image analysis (OBIA) for estimation of substrate changes in a post-bleaching scenario on a maldivian reef

L Fallati, L Saponari, A Savini, F Marchese, C Corselli… - Remote Sensing, 2020 - mdpi.com
Coral reefs are declining worldwide as a result of the effects of multiple natural and
anthropogenic stressors, including regional-scale temperature-induced coral bleaching …

Dyke-induced graben formation in a heterogeneous succession on Mt. Etna: Insights from field observations and FEM numerical models

K Drymoni, E Russo, A Tibaldi, N Corti… - Journal of Volcanology …, 2023 - Elsevier
The most common way of magma transfer towards the surface is through dyking. Dykes can
generate stresses at their tips and the surrounding host rock, initiating surficial deformation …

[HTML][HTML] Volcano-tectonic interactions at the southern margin of the Okataina Volcanic Centre, Taupō Volcanic Zone, New Zealand

K Berryman, P Villamor, I Nairn, J Begg… - Journal of Volcanology …, 2022 - Elsevier
The c. 15 km-long Ngapouri-Rotomahana Fault (NRF) is a major splay of the Paeroa Fault at
the eastern margin of the modern Taupō Rift, the active tectonic structure embedded within …

Surface deformation during the 1928 fissure eruption of Mt. Etna (Italy): Insights from field data and FEM numerical modelling

A Tibaldi, FL Bonali, N Corti, E Russo, K Drymoni… - Tectonophysics, 2022 - Elsevier
The 1928 CE volcanic activity on eastern Etna, Italy, produced wide surface deformation and
high effusion rates along fissures, with excess volumes of about 50 million m 3 of lavas. This …

The Taverna San Felice Dike (NE of Roccamonfina Volcano): Unraveling Magmatic Intrusion Processes and Volcano‐Tectonics in the Tyrrhenian Margin of the …

J Natale, S Vitale, G Giordano, L Fedele… - Geochemistry …, 2023 - Wiley Online Library
The Roccamonfina volcano is located within the Garigliano Graben (southern Apennines,
Italy) and has been active throughout the Middle‐Late Pleistocene. Along its polyphase …

A step forward to understanding the development of volcanotectonic rifts: the structure of the Fremrinamar Fissure Swarm (Iceland)

M Pedicini, FL Bonali, N Corti… - Frontiers in Earth …, 2023 - frontiersin.org
We analysed all the Holocene structures defining the Fremrinamar Fissure Swarm (FFS), in
the Northern Volcanic Zone of Iceland, through the interpretation of aerial photos …

[HTML][HTML] 3D study of dyke-induced asymmetric graben: The 1971 Mt. Etna (Italy) case by structural data and numerical modelling

FL Bonali, N Corti, FP Mariotto, E De Beni… - Journal of Structural …, 2024 - Elsevier
In this work, we have integrated field data and numerical models to characterise a unique
dyke-induced graben system, exposed both in section and plan view, with an unexpected …

Spatio-temporal associations between dike intrusions and fault ruptures in the Tongariro Volcanic Center, New Zealand

MG Gómez-Vasconcelos, P Villamor, SJ Cronin… - Journal of Volcanology …, 2020 - Elsevier
Crustal extension of the southern portion of the Taupo Rift in the Central North Island of New
Zealand is mostly accommodated by normal faulting and rare dike intrusions. To better …

Field evidence of the interplay between rift and transform structures in the Krafla geothermal area, N-Iceland

D Liotta, A Brogi, S Árnadóttir, K Ágústsson… - Geothermics, 2021 - Elsevier
The Krafla volcano-geothermal area is located in Northeast Iceland, within the active
Northern Volcanic Zone sector of the axial rift and has experienced two eruptions in …

Reconstruction of Late Pleistocene-Holocene Deformation through Massive Data Collection at Krafla Rift (NE Iceland) Owing to Drone-Based Structure-from-Motion …

FL Bonali, A Tibaldi, N Corti, L Fallati, E Russo - Applied Sciences, 2020 - mdpi.com
In the present work, we demonstrate how drone surveys coupled with structure-from-motion
(SfM) photogrammetry can help to collect huge amounts of very detailed data even in rough …