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Rimkorolgite

A valid IMA mineral species
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About RimkorolgiteHide

07554220017642005499054.jpg
Olga M. Rimskaya-Korsakova
Formula:
(Mg,Mn)5(Ba,Sr,Ca)(PO4)4 · 8H2O
Colour:
Yellow-brown, light pink, flesh-red to reddish brown
Lustre:
Vitreous, Silky
Hardness:
3
Specific Gravity:
2.67
Crystal System:
Orthorhombic
Name:
Named in honor of Rimskaya-Korsakova, Olga Mikhailovna (Oльга Михайловна Римская-Корсакова) (29 April 1914, St. Petersburg - 18 October 1987), a Russian mineralogist from St. Petersburg University. She was an expert on the Kovdor area, doing 25 years of field work there.
Structurally related to bakhchisaraitsevite and liversidgeite.

15-20% of the grains bear intergrowths with hexagonal polymorph, UM1995-23-PO:BaHMgSr.


Unique IdentifiersHide

Mindat ID:
3420
Long-form identifier:
mindat:1:1:3420:9

IMA Classification of RimkorolgiteHide

Classification of RimkorolgiteHide

8.CH.45

8 : PHOSPHATES, ARSENATES, VANADATES
C : Phosphates without additional anions, with H2O
H : With large and medium-sized cations, RO4:H2O < 1:1

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference for Standard
RolgIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of RimkorolgiteHide

Vitreous, Silky
Transparency:
Transparent, Translucent
Comment:
silky in aggregates.
Colour:
Yellow-brown, light pink, flesh-red to reddish brown
Streak:
White
Hardness:
Tenacity:
Brittle
Cleavage:
Perfect
Perfect {001}
Density:
2.67(2) g/cm3 (Measured)    2.62 g/cm3 (Calculated)

Optical Data of RimkorolgiteHide

Type:
Biaxial (+)
RI values:
nα = 1.552(2) nβ = 1.552(2) nγ = 1.558(2)
2V:
Measured: 23° (5)
Max. Birefringence:
δ = 0.006
Based on recorded range of RI values above.

Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.

Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.

Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.

Surface Relief:
Low (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).

This shows the grain boundary and Becke line effect under plane-polarised light, based on the contrast between this mineral's average refractive index and the mounting medium. It does not take into account mineral colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure - the conoscopic view for a grain cut perpendicular to the acute bisectrix, using this mineral's 2V. The two small white dots mark the melatopes - the points where the two optic axes emerge - and are shown only when they fall within the field of view. The coloured bands are isochromatics, and the dark bands are isogyres.

Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
weak to distinct

Chemistry of RimkorolgiteHide

Mindat Formula:
(Mg,Mn)5(Ba,Sr,Ca)(PO4)4 · 8H2O
Element Weights:
Element% weight
O49.049 %
Ba17.542 %
P15.826 %
Mg15.523 %
H2.060 %

Calculated from ideal end-member formula.
O
Ba
P
Mg
H

Crystallography of RimkorolgiteHide

Crystal System:
Orthorhombic
Cell Parameters:
a = 12.829(4) Å, b = 8.335(2) Å, c = 18.312(3) Å
Ratio:
a:b:c = 1.539 : 1 : 2.197
Unit Cell V:
1,958.10 ų (Calculated from Unit Cell)
Z:
4
Morphology:
short prismatic, fibrous, and in crusts.
Comment:
Point Group: 2/m 2/m 2/m or mm2.; Space Group: P cmm, P cm21, or P c2m.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0006928RimkorolgiteKrivovichev S V, Britvin S N, Burns P C, Yakovenchuk V N (2002) Crystal structure of rimkorolgite, Ba[Mg5(H2O)7(PO4)4](H2O), and its comparison with bakhchisaraitsevite European Journal of Mineralogy 14 397-40220020293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
10.51 Å(100)
3.081 Å(78)
2.969 Å(44)
3.054 Å(41)
3.520 Å(34)
2.839 Å(34)
3.874 Å(32)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 4b: Highly evolved igneous rocks>3.0
36 : Carbonatites, kimberlites, and related igneous rocks
Stage 7: Great Oxidation Event<2.4
47a : [Near-surface hydration of prior minerals]
47c : [Carbonates, phosphates, borates, nitrates]

Type Occurrence of RimkorolgiteHide

Synonyms of RimkorolgiteHide

Other Language Names for RimkorolgiteHide

Simplified Chinese:磷钡镁石
Spanish:Rimkorolgita
Traditional Chinese:磷鋇鎂石

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Rimkorolgite associated with NatroliteNa2Al2Si3O10 · 2H2O
1 photo of Rimkorolgite associated with CalciteCaCO3
1 photo of Rimkorolgite associated with BobierriteMg3(PO4)2 · 8H2O

Related Minerals - Strunz-mindat GroupingHide

8.CH.05Natrowalentaite[Fe3+0.5Na0.5(H2O)6][NaAs3+2(Fe3+2.33W6+0.67)(PO4)2O7]Orth. mmm(2/m2/m2/m) : Imma
8.CH.05Walentaite[Mn2+(H2O)6][◻As3+3Fe3+3(PO4)2O7]Orth. mmm(2/m2/m2/m) : Imma
8.CH.05Halilsarpite[Mg(H2O)6][CaAs3+2(Fe3+2.67Mo6+0.33)(AsO4)2O7]Orth. mmm(2/m2/m2/m) : Imma
8.CH.10AnapaiteCa2Fe2+(PO4)2 · 4H2OTric. 1 : P1
8.CH.15PicropharmacoliteCa4Mg(AsO4)2(HAsO4)2 · 11H2OTric. 1 : P1
8.CH.20Dittmarite(NH4)Mg(PO4) · H2OOrth. mm2 : Pmn21
8.CH.20Niahite(NH4)Mn2+(PO4) · H2OOrth. mm2 : Pmn21
8.CH.25TaranakiteK3Al5(PO3OH)6(PO4)2 · 18H2OTrig. 3m(32/m) : R3c
8.CH.25FrancoanelliteK3Al5(PO3OH)6(PO4)2 · 12H2OTrig.
8.CH.25Macivorite(NH4)3Al5(PO3OH)6(PO4)2 · 18H2OTrig. 3m(32/m) : R3c
8.CH.30Schertelite(NH4)2MgH2(PO4)2 · 4H2OOrth. mmm(2/m2/m2/m) : Pbca
8.CH.35Hannayite(NH4)2Mg3H4(PO4)4 · 8H2OTric. 1 : P1
8.CH.40HazeniteKNaMg2(PO4)2 · 14H2OOrth. mmm(2/m2/m2/m)
8.CH.40Struvite-(K)KMg(PO4) · 6H2OOrth. mm2 : Pmn21
8.CH.40Struvite(NH4)Mg(PO4) · 6H2OOrth. mm2 : Pmn21
8.CH.50BakhchisaraitseviteNa2Mg5(PO4)4 · 7H2OMon. 2/m : P21/b
8.CH.55SmolyaninoviteCo3Fe3+2(AsO4)4 · 11H2OOrth.
8.CH.55FahleiteCaZn5Fe3+2(AsO4)6 · 14H2OOrth.
8.CH.60Barahonaite-(Fe)(Ca,Cu,Na,Fe3+,Al)12Fe3+2(AsO4)8(OH,Cl)x · nH2OMon. 2/m : P2/b
8.CH.60Barahonaite-(Al)(Ca,Cu,Na,Fe3+,Al)12Al2(AsO4)8(OH,Cl)x · nH2OMon. 2/m : P2/b
8.CH.70EpifanoviteNaCaCu5(PO4)4[AsO2(OH)2] · 7H2OMon. 2/m : P21/m
8.CH.75Esdanaite-(Ce)NaMnCe(PO4)2 · 4H2OOrth. 222 : P212121

Other InformationHide

Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

Internet Links for RimkorolgiteHide

References for RimkorolgiteHide

Localities for RimkorolgiteHide

Showing 2 localities.

This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.
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Locality ListHide

- This locality has map coordinates listed. - This locality has estimated coordinates. ⓘ - Click for references and further information on this occurrence. ? - Indicates mineral may be doubtful at this locality. - Good crystals or important locality for species. - World class for species or very significant. (TL) - Type Locality for a valid mineral species. (FRL) - First Recorded Locality for everything else (eg varieties). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).

All localities listed without proper references should be considered as questionable.
Russia
 
  • Murmansk Oblast
    • Kovdorsky District
Liferovich et al. (1998) +1 other reference
Britvin et al. (1995) +5 other references
 
and/or  
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