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Ophiolite from
Rocca Nera, Pontechianale, Cuneo Province, Piedmont, Italy


Locality type:Outcrop
Classification
Type:Ophiolite
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Ophiolite data
Locality Data:Click here to view Rocca Nera, Pontechianale, Cuneo Province, Piedmont, Italy
Data Identifiers
Mindat Occurrence Record ID:1410345
Long-form Identifier:1:3:1410345:6
GUID (UUID V4):1792c39e-a836-4660-b497-746b07206fd4
Nearest other occurrences of Ophiolite
1.6km (1.0 miles) Blanchet lakes, Saint-Véran, Briançon, Hautes-Alpes, Provence-Alpes-Côte d'Azur, France
2.0km (1.2 miles) Tour Real, Pontechianale, Cuneo Province, Piedmont, Italy
69.7km (43.3 miles) Roua Mines (Clue de Roua), Daluis, Nice, Alpes-Maritimes, Provence-Alpes-Côte d'Azur, France
70.4km (43.8 miles) Hubac de Jourdan Mine, Daluis, Nice, Alpes-Maritimes, Provence-Alpes-Côte d'Azur, France
References
Reference Search (possible matching items)
Journal (article/letter/editorial)
Rosenbaum and Lister, 2005). This study focuses on the Piedmont zone of the southwestern Alps (Fig. 1a and b)...Cretaceous to Tertiary times (Tricart, 1984). The Piedmont zone includes different levels of the paleo-subduction...observations further to the north in the same Piedmont zone (Agard et al., 2001; Ganne et al., 2005)...domain is structurally above the Monviso eclogitic ophiolite. In this massif, the metasedimentary component...al., 2012; Schwartz et al., 2001). The Monviso ophiolite corresponds to the subduction channel (Guillot
Journal (article/letter/editorial)
MgHe dating to magnetite from an HP-LT alpine ophiolite body (Rocher Blanc) from the Schistes lustrés...and ZFT data to refine the thermal history of an ophiolite related to their exhumation. The MgHe data suggest...associated erosion. With the present Schistes lustrés ophiolite example, we demonstrate that the MgHe method can...data. Here, the MgHe method is applied to an ophiolite from the Schistes lustrés units (Western Alps...crit- ically evaluated in the framework of the ophiolite thermal history constrained by the ZFT and AFT
 
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