Hydrokenoelsmoreite is a hydrous tungsten oxide mineral with formula □2W2O6(H2O). Hydrokenoelsmoreite is a colorless to white, translucent isometric mineral. It has a Mohs hardness of 3, exhibits no cleavage and has a splintery fracture. It has a vitreous to adamantine luster. It is optically isotropic with an index of refraction of n = 2.24. It forms from the oxidation of ferberite within granitic pegmatite dykes and in pegmatitic greisen veins. It has a structure based on a defect pyrochlore lattice (A2B2O6O’).
| Attributes | Values |
|---|
| rdf:type
| |
| rdfs:label
| - Hidrocenoelsmoreïta (ca)
- Hydrokenoelsmoreit (de)
- Hidrokenoelsmoreita (eu)
- Hydrokenoelsmoreite (en)
- Hydrokenoelsmoreite (it)
|
| rdfs:comment
| - La hidrocenoelsmoreïta és un mineral de la classe dels òxids que pertany al . (ca)
- Hydrokenoelsmoreit ist ein selten vorkommendes Mineral aus der Mineralklasse der „Oxide und Hydroxide“. Es kristallisiert im kubischen Kristallsystem mit der idealisierten chemischen Zusammensetzung □2W2O6(H2O). □ stellt dabei eine Leerstelle (Vakanz) auf der entsprechenden Position dar.Hydrokenoelsmoreit entwickelt nur winzige, oktaedrische Kriställchen mit diamantähnlichem Glanz, die farblos, weiß oder gelblich gefärbt sind. Eisenreichere Varietäten zeigen orangefarbene, blassbraune oder schwarze Farbtöne. Wesentlich häufiger sind mikrokristalline, pulverige Aggregate. (de)
- Hidrokenoelsmoreita]] = oxido motako minerala da eta elsmoreite taldearen kidea da. (eu)
- Hydrokenoelsmoreite is a hydrous tungsten oxide mineral with formula □2W2O6(H2O). Hydrokenoelsmoreite is a colorless to white, translucent isometric mineral. It has a Mohs hardness of 3, exhibits no cleavage and has a splintery fracture. It has a vitreous to adamantine luster. It is optically isotropic with an index of refraction of n = 2.24. It forms from the oxidation of ferberite within granitic pegmatite dykes and in pegmatitic greisen veins. It has a structure based on a defect pyrochlore lattice (A2B2O6O’). (en)
- L'hydrokenoelsmoreite è un minerale appartenente al gruppo dell'elsmoreite; prende il nome dalla località in cui è stata scoperta, i giacimenti di stagno presso il villaggio di Elsmore nel Nuovo Galles del Sud, Australia. Chimicamente è un ossido idrato di tungsteno. Si forma per ossidazione della ferberite nei dicchi di pegmatite granitica e nei filoni di greisen pegmatitico. (it)
|
| foaf:name
| |
| name
| |
| foaf:depiction
| |
| dcterms:subject
| |
| Wikipage page ID
| |
| Wikipage revision ID
| |
| Link from a Wikipage to another Wikipage
| |
| Link from a Wikipage to an external page
| |
| sameAs
| |
| streak
| |
| strunz
| |
| tenacity
| |
| dbp:wikiPageUsesTemplate
| |
| thumbnail
| |
| bot
| |
| caption
| - White stolzite grains accent rich yellow veins of Hydrokenoelsmoreite microcrystals (en)
|
| category
| |
| class
| |
| color
| |
| date
| |
| system
| |
| has abstract
| - La hidrocenoelsmoreïta és un mineral de la classe dels òxids que pertany al . (ca)
- Hydrokenoelsmoreit ist ein selten vorkommendes Mineral aus der Mineralklasse der „Oxide und Hydroxide“. Es kristallisiert im kubischen Kristallsystem mit der idealisierten chemischen Zusammensetzung □2W2O6(H2O). □ stellt dabei eine Leerstelle (Vakanz) auf der entsprechenden Position dar.Hydrokenoelsmoreit entwickelt nur winzige, oktaedrische Kriställchen mit diamantähnlichem Glanz, die farblos, weiß oder gelblich gefärbt sind. Eisenreichere Varietäten zeigen orangefarbene, blassbraune oder schwarze Farbtöne. Wesentlich häufiger sind mikrokristalline, pulverige Aggregate. (de)
- Hidrokenoelsmoreita]] = oxido motako minerala da eta elsmoreite taldearen kidea da. (eu)
- Hydrokenoelsmoreite is a hydrous tungsten oxide mineral with formula □2W2O6(H2O). Hydrokenoelsmoreite is a colorless to white, translucent isometric mineral. It has a Mohs hardness of 3, exhibits no cleavage and has a splintery fracture. It has a vitreous to adamantine luster. It is optically isotropic with an index of refraction of n = 2.24. It forms from the oxidation of ferberite within granitic pegmatite dykes and in pegmatitic greisen veins. It has a structure based on a defect pyrochlore lattice (A2B2O6O’). It was first described for an occurrence in Elsmore Hill, New South Wales, Australia from where it takes its name. (en)
- L'hydrokenoelsmoreite è un minerale appartenente al gruppo dell'elsmoreite; prende il nome dalla località in cui è stata scoperta, i giacimenti di stagno presso il villaggio di Elsmore nel Nuovo Galles del Sud, Australia. Chimicamente è un ossido idrato di tungsteno. Si forma per ossidazione della ferberite nei dicchi di pegmatite granitica e nei filoni di greisen pegmatitico. Il nome hydrokenoelsmoreite è stato approvato dall'IMA nel 2010 nell'ambito di una revisione della nomenclatura del supergruppo del pirocloro, precedentemente era conosciuto come elsmoreite se puro, ferritungstite se ricco di ferro (con W>Fe) o alumotungstite se ricco di alluminio (con W>Al). (it)
|
| cleavage
| |
| formula
| |
| fracture
| |
| IMAsymbol
| |
| luster
| |
| mohs
| |
| gold:hypernym
| |
| prov:wasDerivedFrom
| |
![[RDF Data]](/fct/images/sw-rdf-blue.png)
![[cxml]](/fct/images/cxml_doc.png)
![[csv]](/fct/images/csv_doc.png)
![[text]](/fct/images/ntriples_doc.png)
![[turtle]](/fct/images/n3turtle_doc.png)
![[ld+json]](/fct/images/jsonld_doc.png)
![[rdf+json]](/fct/images/json_doc.png)
![[rdf+xml]](/fct/images/xml_doc.png)
![[atom+xml]](/fct/images/atom_doc.png)
![[html]](/fct/images/html_doc.png)
