Chiara Groppo
Biographic Data
| ID | 8537060 |
|---|---|
| NAME | Chiara Groppo |
| GIVEN NAMES | Chiara |
| FAMILY NAME | Groppo |
| SIGNATURE | GROPPO C |
| AFFILIATIONS | University of Turin |
| ORCID | 0000-0002-4174-6613 |
| VERIFIED | No |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 2 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2012 |
| 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…
Geological map of the ultra-high pressure Brossasco-Isasca unit (Western Alps, Italy)
In the southern Dora-Maira Massif, Western Alps, slivers of continental crust with similar lithologies, but recrystallized during the Alpine orogeny at different peak- P conditions, are exposed. They include the Brossasco-Isasca Unit (BIU) where coesite was first discovered in continental crust. A new 1:20, 000-scale geologic map and related cross-sections of the whole BIU and adjoining units is presented, in which the most significant features u…
No prominent works on this page.
Geological map of the ultra-high pressure Brossasco-Isasca unit (Western Alps, Italy)
In the southern Dora-Maira Massif, Western Alps, slivers of continental crust with similar lithologies, but recrystallized during the Alpine orogeny at different peak- P conditions, are exposed. They include the Brossasco-Isasca Unit (BIU) where coesite was first discovered in continental crust. A new 1:20, 000-scale geologic map and related cross-sections of the whole BIU and adjoining units is presented, in which the most significant features u…
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…
Eclogite (2 works) · Geochemistry (2 works) · Geological and Geochemical Analysis (2 works) · Geology (2 works) · Massif (2 works) · Paleontology (2 works) · Subduction (2 works) · Tectonics (2 works) · Alpine orogeny (1 work) · Blueschist (1 work)