Late metamorphic veins with dominant PS-15 polygonal serpentine in the Monte Avic ultramafite
<p>The ultramafic body of Monte Avic (Aosta Valley, Western Alps, Italy) consists of antigorite serpentinite and Ti-clinohumite metadunite. They host late metamorphic veins, up to a couple of centimeters thick, compact, and homogeneous, with a “porcelain” appearance. Vein colors range from yellowish...
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| Autori principali: | , , , , , , , |
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| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Copernicus Publications
2023-05-01
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| Serie: | European Journal of Mineralogy |
| Accesso online: | https://ejm.copernicus.org/articles/35/347/2023/ejm-35-347-2023.pdf |
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