georgbarsanovite
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Georgbarsanovite is a very rare mineral of the eudialyte group, formerly known under unaccepted name as barsanovite, with formula . The original formula was extended to show the presence of cyclic silicate groups and the domination of silicon at the M4 site. "REE", standing for rare earth elements, is dominated by cerium. Georgbarsanovite is characterized in dominance of manganese at the N4 site. It also differs from most other accepted group representatives in its colour. The mineral was found in nepheline pegmatite near Petrelius River, Khibiny massif, Kola Peninsula, Russia. It is named aft
In the Vinony graph
Vinony's link graph records 5 inbound references to georgbarsanovite, and connects out to silicate mineral, potassium and fluorine.
It is catalogued under topics including Calcium minerals, Cyclosilicates and Iron(II) minerals.
Vinony links it to 4 Wikipedia language editions.
Wikidata facts
- Image
- Georgbarsanovite.jpg
Show 8 more facts
- IMA Mineral Symbol
- Gba
- chemical formula
- Na₁₂(Mn,Sr,REE)₃Ca₆Fe²⁺₃Zr₃NbSi₂₅O₇₆Cl₂·H₂O
- Commons category
- Georgbarsanovite
- Nickel-Strunz 9th edition (updated 2009)
- 9.CO.10
- Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
- 9.CO.10
- type locality (geology)
- Khibiny Mountains
- crystal system
- trigonal crystal system
- streak color
- white
via Wikidata · CC0
~2 min read
Encyclopedic overview
2 sectionsContents
- Notes on chemistry
- References
{{infobox mineral | name = Georgbarsanovite | category = Silicate mineral, Cyclosilicate | image = Georgbarsanovite.jpg | imagesize = | alt = | caption = Georgbarsanovite | formula = {{chem2|Na12(Mn,Sr,REE)3Ca6Fe3^{2+}Zr3NbSi25O76Cl2*H2O}} (original form) | IMAsymbol = Gba | strunz = 9.CO.10 (10 ed) 8/E.23-15 (8 ed) | dana = 64.1.2.2 | system = Trigonal | class = Ditrigonal pyramidal (3m) (same H-M symbol) | symmetry = R3m | unit cell = a = 14.26, c = 29.95 [Å] (approximated); Z = 3 | color = Yellow-green | colour = | habit = pseudo-octahedra | twinning = | cleavage = No | fracture = Uneven | tenacity = Brittle | mohs = | luster = Vitreous | streak = White | diaphaneity = Transparent | gravity = | density = | polish = | opticalprop = Uniaxial (-) | refractive = nω 1.64, nε=1.63 (approximated) | birefringence = | pleochroism = green to pale yellow | 2V = | dispersion = | extinction = | length fast/slow = | fluorescence = | absorption = | melt = | fusibility = | diagnostic = | solubility = | impurities = F, K, Y | alteration = | other = | references = }} Georgbarsanovite is a very rare mineral of the eudialyte group, formerly known under unaccepted name as barsanovite, with formula {{chem2|Na12(Mn,Sr,REE)3Ca6Fe3^{2+}Zr3NbSi(Si3O9)2(Si9O27)2O4Cl2*H2O}}. The original formula was extended to show the presence of cyclic silicate groups and the domination of silicon at the M4 site. "REE", standing for rare earth elements, is dominated by cerium. Georgbarsanovite is characterized in dominance of manganese at the N4 site. It also differs from most other accepted group representatives in its colour. The mineral was found in nepheline pegmatite near Petrelius River, Khibiny massif, Kola Peninsula, Russia. It is named after Russian mineralogist Georg Barsanov.
==Notes on chemistry== Georgbarsanovite contains admixtures of fluorine, potassium and yttrium, with traces of titanium, hafnium, and barium.
Excerpted from Wikipedia’s “georgbarsanovite” article, available under the CC BY-SA 4.0 licence.