[HTML][HTML] Evaluation of an innovative, open-source and quantitative approach for the kinematic analysis of rock slopes based on UAV based Digital Outcrop Model: A …
M Perozzo, N Menegoni, M Foletti, E Poggi… - Engineering …, 2024 - Elsevier
This paper presents a novel, cost-effective method for a rapid and quantitative
characterization of discontinuities in fractured rock cliffs using Unmanned Aerial Vehicle …
characterization of discontinuities in fractured rock cliffs using Unmanned Aerial Vehicle …
[HTML][HTML] Concurrence of load-and-flame structures, balls-and-pillows, clastic injectites and shear deformation bands as indicator of seismicity in mixed siliciclastic …
P Mueller, S Tamburelli, N Menegoni, M Perozzo… - Marine and Petroleum …, 2023 - Elsevier
The present research explores a diverse suite of soft sediment deformation structures
(SSDS) combined with clastic dykes and shear deformation bands distributed throughout a …
(SSDS) combined with clastic dykes and shear deformation bands distributed throughout a …
HTLP metamorphism and fluid‐fluxed melting during multistage anatexis of continental crust (N Sardinia, Italy)
The Variscan high‐grade metamorphic basement of northern Sardinia and southern Corsica
record lower Carboniferous anatexis related to post‐collisional decompression of the …
record lower Carboniferous anatexis related to post‐collisional decompression of the …
Anatomy of a km-scale fault zone controlling the Oligo-Miocene bending of the Ligurian Alps (NW Italy): integration of field and 3D high-resolution digital outcrop …
L Manna, M Perozzo, N Menegoni, S Tamburelli… - Swiss Journal of …, 2023 - Springer
We report the first description of a~ 15 km long NE-SW-striking transtensive fault network
crosscutting the metamorphic units of the Ligurian Alps. The main fault zone, hereby named …
crosscutting the metamorphic units of the Ligurian Alps. The main fault zone, hereby named …
Tectono-metamorphic evolution of a post-variscan mid-crustal shear zone in relation to the Tethyan rifting (Ivrea-Verbano Zone, Southern Alps)
Abstract The Ivrea-Verbano Zone, in the Italian Southern Alps, samples a complete section
of middle to lower continental crust, which records the transition between the Variscan and …
of middle to lower continental crust, which records the transition between the Variscan and …
The role of mantle upwelling on the thermal history of the Tertiary‐Piedmont Basin at the Alps‐Apennines tectonic boundary
Abstract The Tertiary‐Piedmont Basin (NW Italy) is an episutural basin that developed from
the late Eocene on the Alps–Apennines tectonic junction. Several coeval geodynamic …
the late Eocene on the Alps–Apennines tectonic junction. Several coeval geodynamic …
High‐Temperature Strain Localization and the Nucleation of Oceanic Core Complexes (16.5° N, Mid‐Atlantic Ridge)
Extension at slow to ultraslow midoceanic ridges is mostly accommodated by large
detachment faults that expose mantle peridotite and/or lower‐crustal rocks forming Oceanic …
detachment faults that expose mantle peridotite and/or lower‐crustal rocks forming Oceanic …
Sheath fold development around deformable inclusions: Integration of field-analysis (Cima Lunga unit, Central Alps) and 3D numerical models
We investigated complex tectonic structures within a km-scale shear zone (Cima Lunga
unit), which is traditionally interpreted as generated by multiple, distinct deformation phases …
unit), which is traditionally interpreted as generated by multiple, distinct deformation phases …
Syntectonic magmatism and reactivation of collisional structures during late-Variscan shearing (SW Sardinia, Italy)
The Arbus igneous complex (SW Sardinia, Italy) represents a good example of a short time
lived post-collisional composite pluton emplaced at shallow crustal level in the external zone …
lived post-collisional composite pluton emplaced at shallow crustal level in the external zone …
Implications of new geological mapping and U‐Pb zircon dating for the Barrovian tectono‐metamorphic evolution of the Lepontine dome (Central European Alps)
The Barrovian metamorphism of the Lepontine dome is manifested by isograds that cross‐
cut tectonic nappe contacts, which is commonly interpreted as metamorphism that occurred …
cut tectonic nappe contacts, which is commonly interpreted as metamorphism that occurred …