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Cafetite is a rare titanium oxide mineral with formula (Ca,Mg)(Fe,Al)2Ti4O12·4(H2O). It is named for its composition, Ca-Fe-Ti. It was first described in 1959 for an occurrence in the , Afrikanda, Kola Peninsula, Murmanskaja Oblast, Northern Region, Russia. It is also reported from the Khibiny and massifs of the Kola Peninsula and from Meagher County, Montana, US. It occurs in pegmatites in a pyroxenite intrusion as crystals in miarolitic cavities. It occurs associated with ilmenite, titaniferous magnetite, titanite, anatase, perovskite, baddeleyite, phlogopite, clinochlore and kassite.

AttributesValues
rdf:type
rdfs:label
  • Cafetite (en)
  • Cafetita (ca)
  • Cafetit (de)
  • Kafetita (eu)
  • Cafetita (es)
  • Cafetite (it)
rdfs:comment
  • La cafetita és un mineral de la classe dels òxids. (ca)
  • Cafetit ist ein sehr selten vorkommendes Mineral aus der Mineralklasse der „Oxide und Hydroxide“ mit der idealisierten chemischen Zusammensetzung CaTi2O5·H2O und ist damit chemisch gesehen ein wasserhaltiges Calcium-Titan-Oxid. Cafetit kristallisiert im monoklinen Kristallsystem und entwickelt meist nadelige bis säulige Kristalle mit gestreiften Prismenflächen. Daneben findet er sich auch in Form faseriger, verworrener Mineral-Aggregate und Massen. Die durchsichtigen bis durchscheinenden Kristalle sind meist hellgelb bis farblos, können aber auch eine orangebraune Farbe annehmen. (de)
  • Cafetite is a rare titanium oxide mineral with formula (Ca,Mg)(Fe,Al)2Ti4O12·4(H2O). It is named for its composition, Ca-Fe-Ti. It was first described in 1959 for an occurrence in the , Afrikanda, Kola Peninsula, Murmanskaja Oblast, Northern Region, Russia. It is also reported from the Khibiny and massifs of the Kola Peninsula and from Meagher County, Montana, US. It occurs in pegmatites in a pyroxenite intrusion as crystals in miarolitic cavities. It occurs associated with ilmenite, titaniferous magnetite, titanite, anatase, perovskite, baddeleyite, phlogopite, clinochlore and kassite. (en)
  • La cafetita es la forma mineral de un hidróxido de fórmula química CaTi2O5·H2O.Fue descubierta por Aleksandr Kukharenko y colaboradores en el macizo ultrabásico de (península de Kola, Rusia) en 1959.​Originalmente su composición fue referida como (Ca,Mg)(Fe,Al)2Ti4O12·4H2O.Aunque actualmente se considera que el hierro no es esencial, el nombre de este mineral hace alusión a su composición, CAlcio, hierro (en latín = FErrum) y TItanio.​​ (es)
  • Kafetita oxido motako minerala da. (eu)
  • La cafetite è un minerale. (it)
foaf:name
  • Cafetite (en)
name
  • Cafetite (en)
foaf:depiction
  • http://commons.wikimedia.org/wiki/Special:FilePath/Cafetite,_Lizardite,_Calcite-529437.jpg
dcterms:subject
Wikipage page ID
Wikipage revision ID
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sameAs
streak
  • White (en)
strunz
tenacity
  • Brittle (en)
unit cell
  • a = 4.944 Å, (en)
  • b = 12.109 Å, (en)
  • c = 15.911 Å; (en)
  • β= 98.93°; Z = 8 (en)
dbp:wikiPageUsesTemplate
thumbnail
caption
  • Yellow cafetite crystals with green lizardite and calcite (en)
category
class
  • Prismatic (en)
color
  • Pale yellow to colorless (en)
gravity
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