dbo:abstract | - La ferrokentbrooksita és un mineral de la classe dels silicats, que pertany al . Rep el nom per ser l'anàleg amb ferro dominant la kentbrooksita. (ca)
- Ferrokentbrooksite is a moderately rare mineral of the eudialyte group, with formula Na15Ca6(Fe,Mn)3Zr3NbSi25O73(O,OH,H2O)3(Cl,F,OH)2. The original formula was extended form to show the presence of cyclic silicate groups and presence of silicon at the M4 site, according to the nomenclature of eudialyte group. As suggested by its name, it is the (ferrous) iron analogue of kentbrooksite. When compared to the latter, it is also chlorine-dominant instead of being fluorine-dominant. The original (holotype) material is also relatively enriched in rare earth elements, including cerium and yttrium. (en)
- Ferrokentbrooksita silikato motako minerala da eta eudialyte taldearen kidea da. (eu)
- La ferrokentbrooksite è un minerale appartenente al gruppo dell'eudialite. (it)
|
dbo:thumbnail | |
dbo:wikiPageID | |
dbo:wikiPageLength | - 4510 (xsd:nonNegativeInteger)
|
dbo:wikiPageRevisionID | |
dbo:wikiPageWikiLink | |
dbp:caption | - Ferrokentbrooksite, Amphibole Supergroup-166795 (en)
|
dbp:category | |
dbp:class | |
dbp:cleavage | |
dbp:color | - Reddish brown to red (en)
|
dbp:dana | |
dbp:diaphaneity | |
dbp:fracture | - Uneven to conchoidal (en)
|
dbp:habit | |
dbp:imasymbol | |
dbp:impurities | |
dbp:luster | |
dbp:name | |
dbp:refractive | |
dbp:streak | |
dbp:strunz | - 9 (xsd:integer)
- (8/E.23-15 ) (en)
|
dbp:symmetry | |
dbp:system | |
dbp:unitCell | - a = 14.25, c = 30.03 [Å] ; Z = 3 (en)
|
dbp:wikiPageUsesTemplate | |
dcterms:subject | |
rdf:type | |
rdfs:comment | - La ferrokentbrooksita és un mineral de la classe dels silicats, que pertany al . Rep el nom per ser l'anàleg amb ferro dominant la kentbrooksita. (ca)
- Ferrokentbrooksite is a moderately rare mineral of the eudialyte group, with formula Na15Ca6(Fe,Mn)3Zr3NbSi25O73(O,OH,H2O)3(Cl,F,OH)2. The original formula was extended form to show the presence of cyclic silicate groups and presence of silicon at the M4 site, according to the nomenclature of eudialyte group. As suggested by its name, it is the (ferrous) iron analogue of kentbrooksite. When compared to the latter, it is also chlorine-dominant instead of being fluorine-dominant. The original (holotype) material is also relatively enriched in rare earth elements, including cerium and yttrium. (en)
- Ferrokentbrooksita silikato motako minerala da eta eudialyte taldearen kidea da. (eu)
- La ferrokentbrooksite è un minerale appartenente al gruppo dell'eudialite. (it)
|
rdfs:label | - Ferrokentbrooksita (ca)
- Ferrokentbrooksite (en)
- Ferrokentbrooksita (eu)
- Ferrokentbrooksite (it)
|
owl:sameAs | |
prov:wasDerivedFrom | |
foaf:depiction | |
foaf:isPrimaryTopicOf | |
foaf:name | |
isdbo:wikiPageWikiLink of | |
isfoaf:primaryTopic of | |