Marco Gattiglio
Biographic Data
| ID | 7516422 |
|---|---|
| NAME | Marco Gattiglio |
| GIVEN NAMES | Marco |
| FAMILY NAME | Gattiglio |
| SIGNATURE | GATTIGLIO M |
| AFFILIATIONS | University of Turin |
| ORCID | 0000-0002-1885-2872 |
| VERIFIED | Yes |
| TOTAL WORKS | 7 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 7 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2011 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 0 |
Tectonic setting of the Susa and Lanzo Valleys Ophiolites (Western Alps)
The 1:30,000 scale geological map of the Viù Valley (∼200 km2) depicts the tectonic architecture of the Susa and Lanzo Valleys Ophiolites (SLVO), a slice of the Jurassic Ligurian-Piedmont oceanic lithosphere stacked in the Western Alps. The SLVO successions (i.e. serpentinite, metagabbro, metabasalt and metasediments) were subducted, metamorphosed under high-pressure conditions, and exhumed during the Alpine orogeny. Detailed mapping and structur…
Tectonic relationships between the Paleozoic basement and the Mesozoic cover succession in the northern Dora-Maira Massif (Susa Valley, Western Alps)
The northernmost sector of the Dora-Maira Massif is a key area for studying the role of basement-cover detachment zones as markers for understanding the multistage tectonic evolution of orogenic belts. The 1:5,000 scale geological map highlights the tectonic relationships between the Paleozoic basement and Mesozoic cover successions, which are separated by the Bussoleno Detachment Shear Zone, representing the basement-cover interface, and are tec…
Geology of the Monte Banchetta – Punta Rognosa area (Troncea valley, Western Alps)
The map ‘Geology of the Monte Banchetta – Punta Rognosa area (Troncea valley, Western Alps)’ details the lithostratigraphy and structural setting of a key sector in the Alpine chain, characterized by close associations of continental and oceanic basements, and meta-sediments. The mapped Monte Banchetta – Punta Rognosa unit (BRU), tectonically juxtaposed to different metaophiolitic units, comprises the Punta Rognosa succession, made of serpentiniz…
Deep-seated gravitational slope deformation involving glacial evidence in the Rodoretto Valley (NW Alps)
The Rodoretto Valley (about 25 km2) (Western Alps, NW Italy) shaped in the metamorphic bedrock, covered by Quaternary sediments, is involved in significant deep-seated gravitational slope deformation (DSGSD). A detailed field survey revealed several morpho-structures typically related to DSGSD phenomena (open fractures, doubled ridges, scarps, trenches, counterscarps and bulging reliefs) and other significant gravitational morphologies, here defi…
Geology of the Susa Shear Zone (Susa Valley, Western Alps)
The 1:10,000 scale geological map of the Susa Shear Zone (SSZ) in the inner sector of the Western Alps, aims to describe the geological setting and tectonic evolution of a first-order Alpine shear zone, which drove exhumation and juxtaposition of different oceanic and continental margin units (i.e. the blueschist-facies External Piedmont Zone in its hanging wall and the eclogite-facies Internal Piedmont Zone and Dora Maira Massif in its footwall)…
Deep-seated gravitational slope deformations as possible suitable locations for prehistoric human settlements
Geological map of the middle Orco Valley, Western Italian Alps
Please click here to download the map associated with this article. Detailed mapping of the middle Orco Valley in the Western Italian Alps allowed for the reconstruction of the lithostratigraphy and the structural evolution of different tectonic units along a geological section from the Gran Paradiso Massif to the Gneiss Minuti Complex of the Sesia-Lanzo Zone. The studied nappes can be grouped into a Lower Tectonic Element which underwent eclogit…
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Geological map of the middle Orco Valley, Western Italian Alps
Please click here to download the map associated with this article. Detailed mapping of the middle Orco Valley in the Western Italian Alps allowed for the reconstruction of the lithostratigraphy and the structural evolution of different tectonic units along a geological section from the Gran Paradiso Massif to the Gneiss Minuti Complex of the Sesia-Lanzo Zone. The studied nappes can be grouped into a Lower Tectonic Element which underwent eclogit…
Deep-seated gravitational slope deformations as possible suitable locations for prehistoric human settlements
Geology of the Susa Shear Zone (Susa Valley, Western Alps)
The 1:10,000 scale geological map of the Susa Shear Zone (SSZ) in the inner sector of the Western Alps, aims to describe the geological setting and tectonic evolution of a first-order Alpine shear zone, which drove exhumation and juxtaposition of different oceanic and continental margin units (i.e. the blueschist-facies External Piedmont Zone in its hanging wall and the eclogite-facies Internal Piedmont Zone and Dora Maira Massif in its footwall)…
Geology of the Monte Banchetta – Punta Rognosa area (Troncea valley, Western Alps)
The map ‘Geology of the Monte Banchetta – Punta Rognosa area (Troncea valley, Western Alps)’ details the lithostratigraphy and structural setting of a key sector in the Alpine chain, characterized by close associations of continental and oceanic basements, and meta-sediments. The mapped Monte Banchetta – Punta Rognosa unit (BRU), tectonically juxtaposed to different metaophiolitic units, comprises the Punta Rognosa succession, made of serpentiniz…
Deep-seated gravitational slope deformation involving glacial evidence in the Rodoretto Valley (NW Alps)
The Rodoretto Valley (about 25 km2) (Western Alps, NW Italy) shaped in the metamorphic bedrock, covered by Quaternary sediments, is involved in significant deep-seated gravitational slope deformation (DSGSD). A detailed field survey revealed several morpho-structures typically related to DSGSD phenomena (open fractures, doubled ridges, scarps, trenches, counterscarps and bulging reliefs) and other significant gravitational morphologies, here defi…
Tectonic relationships between the Paleozoic basement and the Mesozoic cover succession in the northern Dora-Maira Massif (Susa Valley, Western Alps)
The northernmost sector of the Dora-Maira Massif is a key area for studying the role of basement-cover detachment zones as markers for understanding the multistage tectonic evolution of orogenic belts. The 1:5,000 scale geological map highlights the tectonic relationships between the Paleozoic basement and Mesozoic cover successions, which are separated by the Bussoleno Detachment Shear Zone, representing the basement-cover interface, and are tec…
Tectonic setting of the Susa and Lanzo Valleys Ophiolites (Western Alps)
The 1:30,000 scale geological map of the Viù Valley (∼200 km2) depicts the tectonic architecture of the Susa and Lanzo Valleys Ophiolites (SLVO), a slice of the Jurassic Ligurian-Piedmont oceanic lithosphere stacked in the Western Alps. The SLVO successions (i.e. serpentinite, metagabbro, metabasalt and metasediments) were subducted, metamorphosed under high-pressure conditions, and exhumed during the Alpine orogeny. Detailed mapping and structur…
Geology (6 works) · Geomorphology (6 works) · Geology and Paleoclimatology Research (5 works) · Tectonics (5 works) · Geological and Geochemical Analysis (4 works) · Paleontology (4 works) · Geochemistry (3 works) · Geography (3 works) · Geological and Geophysical Studies Worldwide (3 works) · Massif (3 works)