Paola Cadoppi
Biographic Data
| ID | 8537340 |
|---|---|
| NAME | Paola Cadoppi |
| GIVEN NAMES | Paola |
| FAMILY NAME | Cadoppi |
| SIGNATURE | CADOPPI P |
| AFFILIATIONS | University of Turin |
| VERIFIED | No |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 2 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2016 |
| LATEST PUBLICATION YEAR | 2020 |
| H-INDEX | 0 |
Geology of the southern Dora-Maira Massif
In the Valmala sector of the southern Dora Maira Massif (Western Alps), two different eclogite- and blueschist-facies units (i.e. the Rocca Solei and Dronero units, respectively), are separated by a shear zone (i.e. the Valmala Tectonic Unit), which peculiarly consists of mixed slices of ophiolitic and continental rocks. A detailed geological map at 1:10,000 scale allowed to point out that the tectonic slices within the Valmala Tectonic Unit cons…
Geology of the Fontane talc mineralization (Germanasca valley, Italian Western Alps)
The 1:5000 scale Geological Map of the Fontane talc mineralization (FTM) aims to give new information about the origin and geological structure of an important talc mineralization occurring in the axial sector of the Italian Western Alps. The FTM is hosted within a pre-Carboniferous polymetamorphic complex which was deformed and metamorphosed during both Variscan and Alpine orogenesis, and is part of the Dora-Maira continental crust. Field mappin…
No prominent works on this page.
Geology of the Fontane talc mineralization (Germanasca valley, Italian Western Alps)
The 1:5000 scale Geological Map of the Fontane talc mineralization (FTM) aims to give new information about the origin and geological structure of an important talc mineralization occurring in the axial sector of the Italian Western Alps. The FTM is hosted within a pre-Carboniferous polymetamorphic complex which was deformed and metamorphosed during both Variscan and Alpine orogenesis, and is part of the Dora-Maira continental crust. Field mappin…
Geology of the southern Dora-Maira Massif
In the Valmala sector of the southern Dora Maira Massif (Western Alps), two different eclogite- and blueschist-facies units (i.e. the Rocca Solei and Dronero units, respectively), are separated by a shear zone (i.e. the Valmala Tectonic Unit), which peculiarly consists of mixed slices of ophiolitic and continental rocks. A detailed geological map at 1:10,000 scale allowed to point out that the tectonic slices within the Valmala Tectonic Unit cons…
Geochemistry (2 works) · Geological and Geochemical Analysis (2 works) · Geology (2 works) · Geology and Paleoclimatology Research (2 works) · Paleontology (2 works) · Tectonics (2 works) · Blueschist (1 works) · Carboniferous (1 works) · Continental crust (1 works) · Continental Margin (1 works)