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Roymillerite

A valid IMA mineral species
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About RoymilleriteHide

00570970017272472892095.jpg
Roy Miller
Formula:
Pb24Mg9(Si10O28)(CO3)10(BO3)(SiO4)(OH)13O5
Colour:
Colourless to light pink
Lustre:
Vitreous
Specific Gravity:
5.973 (Calculated)
Crystal System:
Triclinic
Name:
Named for dr Roy McG. Miller for his contributions to the knowledge of the Namibia's geology
Chemically quite similar to britvinite; structurally related to britvinite and molybdophyllite. The combination of anion types in roymillerite is unique.

Crystal structure details:
- pyrophyllite-type TOT-modules of the Mg9(OH)8[(Si,Al)10O28] composition
- I-blocks of the Pb24(OH)6O4(CO3)10(BO3,SiO4) composition


Unique IdentifiersHide

Mindat ID:
50357
Long-form identifier:
mindat:1:1:50357:6

IMA Classification of RoymilleriteHide

Classification of RoymilleriteHide

9.EG.70

9 : SILICATES (Germanates)
E : Phyllosilicates
G : Double nets with 6-membered and larger rings

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

Physical Properties of RoymilleriteHide

Vitreous
Transparency:
Transparent
Comment:
strong
Colour:
Colourless to light pink
Cleavage:
Perfect
on (001)
Density:
5.973 g/cm3 (Calculated)

Optical Data of RoymilleriteHide

Type:
Biaxial (-)
RI values:
nα = 1.86(1) nβ = 1.94(1) nγ = 1.94(1)
2V:
Measured: 5° (5)
Max. Birefringence:
δ = 0.080
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:
Very High (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.

Chemistry of RoymilleriteHide

Mindat Formula:
Pb24Mg9(Si10O28)(CO3)10(BO3)(SiO4)(OH)13O5
Element Weights:
Element% weight
Pb71.321 %
O19.046 %
Si4.431 %
Mg3.137 %
C1.723 %
H0.188 %
B0.155 %

Calculated from ideal end-member formula.
Pb
O
Si
Mg
C
H
B

Crystallography of RoymilleriteHide

Crystal System:
Triclinic
Class (H-M):
1 - Pinacoidal
Space Group:
P1
Cell Parameters:
a = 9.316(1) Å, b = 9.316(1) Å, c = 26.463(4) Å
α = 83.295(3)°, β = 83.308(3)°, γ = 60.023(2)°
Ratio:
a:b:c = 1 : 1 : 2.841
Unit Cell V:
1971.2 ų
Z:
1
Morphology:
Platy single-crystal grains

X-Ray Powder DiffractionHide

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
High-? alteration and/or metamorphism
31 : Thermally altered carbonate, phosphate, and iron formations

Type Occurrence of RoymilleriteHide

General Appearance of Type Material:
Platy single-crystal grains, up to 1.5 x 0.3 mm in size
Place of Conservation of Type Material:
Cotype: mineralogical collections of the Swedish Museum of Natural History, Stockholm, Sweden (catalogue # 20080176)
Empirical Formula of Type Material:
Pb24.12Mg8.74Mn1.25Fe0.94B1.03Al1.04C9.46Si9.39H14.27O83
Chemical Analysis of Type Material:
MgO4.93 %
MnO1.24 %
FeO0.95 %
PbO75.38 %
B2O30.50 %
Al2O30.74 %
CO25.83 %
SiO27.90 %
H2O1.8 %
Total:99.27 %
Associated Minerals at Type Locality:

Synonyms of RoymilleriteHide

Other Language Names for RoymilleriteHide

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Roymillerite associated with RhodochrositeMnCO3
1 photo of Roymillerite associated with CerussitePbCO3
1 photo of Roymillerite associated with JacobsiteMn2+Fe3+2O4

Related Minerals - Strunz-mindat GroupingHide

9.EG.05CymriteBaAl2Si2(O,OH)8 · H2OMon. 2 : P21
9.EG.10Naujakasite(Na,K)6(Fe2+,Mn2+,Ca)(Al,Fe)4Si8O26Mon.
9.EG.10ManganonaujakasiteNa6(Mn2+,Fe2+)Al4Si8O26Mon. 2/m : B2/m
9.EG.15DmisteinbergiteCa(Al2Si2O8)Trig. 32 : P312
9.EG.20KampfiteBa12(Si11Al5)O31(CO3)8Cl5Mon. m
9.EG.25VertumniteCa4Al4Si4O6(OH)24 · 3H2OMon. 2/m : P21/m
9.EG.30Eggletonite(Na,K,Ca)xMn6(Si,Al)10O24(OH)4 · nH2O (x = 1-2; n = 7-11)Mon.
9.EG.30Ganophyllite(K,Na)xMn2+6(Si,Al)10O24(OH)4 · nH2O (x = 1-2; n = 7-11)Mon. 2/m : B2/b
9.EG.30Tamaite(Ca,K,Na)xMn6(Si,Al)10O24(OH)4 · nH2O (x = 1-2; n = 7-11)Mon. 2/m : P21/c
9.EG.35ZussmaniteK(Fe,Mg,Mn)13(Si,Al)18O42(OH)14Trig. 3 : R3
9.EG.35CoombsiteKMn2+13(Si,Al)18O42(OH)14Trig.
9.EG.40'Chalcodite'K(Fe3+,Mg,Fe2+)8(Si,Al)12(O,OH)27Tric. 1 : P1
9.EG.40Parsettensite(K,Na,Ca)7.5(Mn,Mg)49Si72O168(OH)50 · nH2OMon. 2/m : B2/m
9.EG.40LennilenapeiteK4Mn2+48[Si64Al8]O164(OH)52 · nH2OTric.
9.EG.40StilpnomelaneK4Fe2+48[Si64Al8]O164(OH)52 · nH2OTric. 1 : P1
9.EG.45Latiumite(Ca,K)4(Si,Al)5O11(SO4,CO3)Mon. 2 : P21
9.EG.45LevantiteKCa3Al2(SiO4)(Si2O7)(PO4)Mon. 2 : P21
9.EG.45TuscaniteKCa6(Si,Al)10O22(SO4,CO3)2(OH) · H2OMon. 2/m : P21/c
9.EG.50JagoitePb18Fe3+4[Si4(Si,Fe3+)6][Pb4Si16(Si,Fe)4]O82Cl6Hex. 6m2 : P6c2
9.EG.50FriisitePb8Al3Si8O27Cl3Hex. 6m2 : P62c
9.EG.55WickenburgiteCaPb3Al2Si10O24(OH)6Trig. 3m : P31c
9.EG.60HyttsjöitePb18Ba2Ca5Mn2+2Fe3+2Si30O90Cl · 6H2OTrig. 3 : R3
9.EG.65ArmbrusteriteK5Na7Mn15[(Si9O22)4](OH)10 · 4H2OMon. 2/m : B2/m
9.EG.70Britvinite[Pb7(OH)3F(BO3)2(CO3)][Mg4.5(OH)3(Si5O14)]Tric. 1 : P1
9.EG.75KayupovaiteNa2Mn10[(Si14Al2)O38(OH)8] · 7H2OMon. 2/m : B2/b
9.EG.75'UM1989-30-SiO:AlBaCaFeHKMgMn'(Ba,Ca)(Mn,Fe,Mg)22(Si,Al)32O76(OH)16 · 12H2O
9.EG.75BannisteriteCaMn2+10(Si14Al2)O38(OH)8 · nH2OMon. 2/m : B2/b

Other InformationHide

IR Spectrum:
Confirms the presence of the britvinite-type tetrahedral sheets, and the complex anions given in the formula
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 RoymilleriteHide

References for RoymilleriteHide

Localities for RoymilleriteHide

Showing 1 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.
Namibia (TL)
 
  • Otjozondjupa Region
    • Otavi Constituency
      • Kombat
Hålenius et al. (2016) +2 other references
 
and/or  
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