Skip to content
EntityQ3744361· pop 5· linked from 4 articles

Also known as IMA1995-016

Fianelite is a mineral belonging to the manganese vanadate category, found in iron-manganese ores. Named after the place where it was found, Fianel, a mine located in Val Ferrera (Ferrera valley), in the canton of Graubünden, Swiss. This mineral is found in small amounts in metamorphosed iron-manganese ores. This is the last crystallization of vanadate at the site since medaite was the last vanadate mineral being crystallized, but because of retrograde metamorphism, occurring at the place, vanadium moved into medaite veinlets, forming cross-cutting fianelite on medaite.

~4 min read

Encyclopedic overview

8 sections
Contents
  • Occurrence
  • Physical properties
  • Optical properties
  • Chemical properties
  • Chemical composition
  • X-ray crystallography
  • See also
  • References

{{Infobox mineral | name = Fianelite | category = Vanadate | image = | caption = | formula = Mn2V(V,As)O7 · 2H2O | IMAsymbol = Fnl | molweight = | strunz = 08.FC.05 | system = Monoclinic | class = 2/m | symmetry = P21/n | unit cell = a = 7.809;Å, b = 14.554;Å c = 6.705 Å, β = 93.27(3)◦ | color = Orange-Red | habit = Platy | twinning = None observed | cleavage = Good on {001} and {100} | fracture = | tenacity = | mohs = 3 | luster = Vitreous | polish = | refractive = 1.85±0.02 | opticalprop = | birefringence = δ=1.820 | dispersion = Good | pleochroism = | fluorescence= | absorption = | streak = | gravity = 3.22 gm/cc | density = 3.21 g/cm3 | melt = | fusibility = | diagnostic = | solubility = | diaphaneity = Transparent | other = | references = }}

Fianelite is a mineral belonging to the manganese vanadate category, found in iron-manganese ores. Named after the place where it was found, Fianel, a mine located in Val Ferrera (Ferrera valley), in the canton of Graubünden, Swiss. This mineral is found in small amounts in metamorphosed iron-manganese ores. This is the last crystallization of vanadate at the site since medaite was the last vanadate mineral being crystallized, but because of retrograde metamorphism, occurring at the place, vanadium moved into medaite veinlets, forming cross-cutting fianelite on medaite.

Excerpted from Wikipedia’s “fianelite” article, available under the CC BY-SA 4.0 licence.

Available in 4 languages

via Wikidata sitelinks · CC0