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Plavnoite is a rare complex uranium sulfate mineral with the formula K0.8Mn0.6[(UO2)2O2(SO4)]•3.5H2O. Typically for the secondary uranium mineral, plavnoite contains uranyl groups. It was discovered in the Plavno mine in Jáchymov, Czech Republic. The Jáchymov site is known as a type locality for many rare and unique minerals.

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rdf:type
rdfs:label
  • Plavnoïta (ca)
  • Plavnoita (eu)
  • Plavnoite (en)
rdfs:comment
  • La plavnoïta és un mineral de la classe dels sulfats, que partany al grup de la zippeïta. (ca)
  • Plavnoita mineral bat da eta zippeita taldearen kidea da. (eu)
  • Plavnoite is a rare complex uranium sulfate mineral with the formula K0.8Mn0.6[(UO2)2O2(SO4)]•3.5H2O. Typically for the secondary uranium mineral, plavnoite contains uranyl groups. It was discovered in the Plavno mine in Jáchymov, Czech Republic. The Jáchymov site is known as a type locality for many rare and unique minerals. (en)
foaf:name
  • Plavnoite (en)
name
  • Plavnoite (en)
foaf:depiction
  • http://commons.wikimedia.org/wiki/Special:FilePath/Radioactive.svg
dcterms:subject
Wikipage page ID
Wikipage revision ID
Link from a Wikipage to another Wikipage
sameAs
unit cell
  • a = 8.63, b = 14.28, (en)
  • c = 8.86 [Å], β = 104.04° (en)
dbp:wikiPageUsesTemplate
thumbnail
category
class
  • Prismatic (en)
Other
symmetry
  • C2/m (en)
system
has abstract
  • La plavnoïta és un mineral de la classe dels sulfats, que partany al grup de la zippeïta. (ca)
  • Plavnoita mineral bat da eta zippeita taldearen kidea da. (eu)
  • Plavnoite is a rare complex uranium sulfate mineral with the formula K0.8Mn0.6[(UO2)2O2(SO4)]•3.5H2O. Typically for the secondary uranium mineral, plavnoite contains uranyl groups. It was discovered in the Plavno mine in Jáchymov, Czech Republic. The Jáchymov site is known as a type locality for many rare and unique minerals. (en)
formula
  • K0.8Mn0.6[2O2]•3.5H2O (en)
IMAsymbol
  • Pvn (en)
prov:wasDerivedFrom
page length (characters) of wiki page
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is Link from a Wikipage to another Wikipage of
is foaf:primaryTopic of
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