Locality type: | Quarry |
Classification |
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Type: | Orthogneiss |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Orthogneiss data |
Locality Data: | Click here to view Argentera Quarry (Montestrutto Quarry), Settimo Vittone, Metropolitan City of Turin, Piedmont, Italy |
Data Identifiers |
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Mindat Occurrence Record ID: | 1351535 |
Long-form Identifier: | 1:3:1351535:3 |
GUID (UUID V4): | bec3a2d4-76af-421f-abd2-6927eea075e9 |
Nearest other occurrences of Orthogneiss |
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0.3km (0.2 miles) | ⓘMontestrutto glacial terrace, Settimo Vittone, Metropolitan City of Turin, Piedmont, Italy |
83.0km (51.6 miles) | ⓘCannero Riviera ore body, Trarego Viggiona, Verbano-Cusio-Ossola Province, Piedmont, Italy |
83.5km (51.9 miles) | ⓘVal di Crana pegmatites, Val di Crana, Toceno, Verbano-Cusio-Ossola Province, Piedmont, Italy |
91.2km (56.7 miles) | ⓘRio Geronda Valley, Salbertrand, Metropolitan City of Turin, Piedmont, Italy |
References |
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Tropper, P., Essene, E.J., Sharp, Z.D., and Hunziker, J.C. (1999) Application of K-feldspar - jadeite- quartz barometry to eclogite facies metagranites and metapelites in the Sesia Lanzo Zone (Western Alps, Italy). Journal of Metamorphic Geology, 17, 195-209 Liermann, H.-P., Isachsen, C., Altenberger, U., and Oberhänsli, R. (2002) Behavior of zircon during high-pressure, low-temperature metamorphism: Case study from the Internal Unit of the Sesia Zone (Western Italian Alps). European Journal of Mineralogy, 14, 61–71 Compagnoni, R., Engi, M., and Regis, D. (2014) Valle d’Aosta section of the Sesia Zone: multi-stage HP metamorphism and assembly of a rifted continental margin.10th International Eclogite Conference - Courmayeur (Aosta, Italy), 2013. GFT - Geological Field Trips, 6, 1-2, 44 pages. |