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Ribbeite

A valid IMA mineral species
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About RibbeiteHide

07132910017271926231894.jpg
Paul Ribbe
Formula:
Mn2+5(SiO4)2(OH)2
Mn may be replaced by minor Mg.
Colour:
Pink
Lustre:
Vitreous, Sub-Vitreous
Hardness:
5
Specific Gravity:
3.90
Crystal System:
Orthorhombic
Name:
Named in 1987 by Donald R. Peacor, Pete J. Dunn, S. C. Su, and J. Innes in honor of Paul Hubert Ribbe [2 April 1935 Bristol, Connecticut, USA - 24 June 2017 Virginia, USA], professor of mineralogy at Virginia Polytechnic Institute and State University, Blacksburg, Virginia, USA and investigator of crystal structures, particularly those of the feldspar group. The publication of the new species commented: "We have named this new species ribbeite in honor of Dr. Paul H. Ribbe in recognition of his many contributions to mineralogy, both to the science through his research, and to the society of mineralogists, in part through his editorship of the Reviews in Mineralogy series of the Mineralogical Society of America. It is particularly appropriate that ribbeite is closely related to the humite group, to which he has made major contributions."
Dimorph of:
This page provides mineralogical data about Ribbeite.


Unique IdentifiersHide

Mindat ID:
3411
Long-form identifier:
mindat:1:1:3411:7

IMA Classification of RibbeiteHide

Classification of RibbeiteHide

9.AF.65

9 : SILICATES (Germanates)
A : Nesosilicates
F : Nesosilicates with additional anions; cations in [4], [5] and/or only [6] coordination
52.3.2b.4

52 : NESOSILICATES Insular SiO4 Groups and O,OH,F,H2O
3 : Insular SiO4 Groups and O, OH, F, and H2O with cations in [6] coordination only
14.17.5

14 : Silicates not Containing Aluminum
17 : Silicates of Mn

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

Physical Properties of RibbeiteHide

Vitreous, Sub-Vitreous
Transparency:
Transparent
Colour:
Pink
Streak:
White
Hardness:
Tenacity:
Brittle
Cleavage:
None Observed
Fracture:
Irregular/Uneven
Density:
3.90 g/cm3 (Measured)    3.84 g/cm3 (Calculated)

Optical Data of RibbeiteHide

Type:
Biaxial (+)
RI values:
nα = 1.780 nβ = 1.792 nγ = 1.808
2V:
Measured: 83° , Calculated: 84°
Birefringence:
0.028
Max. Birefringence:
δ = 0.028
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:
Moderate
Dispersion:
r > v distinct
Pleochroism:
Visible
Comments:
X, Y colorless; Z light pink
Comments:
Z > X - Y; X = b, Y = a, Z = c

Chemistry of RibbeiteHide

Mindat Formula:
Mn2+5(SiO4)2(OH)2

Mn may be replaced by minor Mg.
Element Weights:
Element% weight
Mn55.733 %
O32.462 %
Si11.397 %
H0.409 %

Calculated from ideal end-member formula.
Common Impurities:
Fe,Ca,H2O

Crystallography of RibbeiteHide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Cell Parameters:
a = 4.799 Å, b = 10.742 Å, c = 15.70 Å
Ratio:
a:b:c = 0.447 : 1 : 1.462
Unit Cell V:
809.35 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Anhedral
Comment:
Space group either Pbnm or Pbn21

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0001545RibbeiteFreed R L, Rouse R C, Peacor D R (1993) Ribbeite, a second example of edge-sharing silicate tetrahedra in the leucophoenicite group American Mineralogist 78 190-19419930293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
5.08 Å(5)
4.41 Å(30)
4.23 Å(2)
3.93 Å(1)
3.83 Å(30)
3.53 Å(5)
3.49 Å(5)
3.362 Å(10)
3.256 Å(5)
2.925 Å(70)
2.873 Å(80)
2.821 Å(70)
2.695 Å(60)
2.552 Å(80)
2.515 Å(40)
2.398 Å(2)
2.356 Å(40)
2.315 Å(5)
2.246 Å(10)
2.216 Å(2)
2.117 Å(5)
1.996 Å(1)
1.834 Å(1)
1.796 Å(100)
Comments:
Peacor, Donald R., Dunn, Pete J., Su, Shu-Chun, and Innes, John (1987) Ribbeite, a Polymorph of Alleghanyite and Member of the Leucophoenicite Group from the Kombat Mine, Namibia, The American Mineralogist, v. 72, p. 213-216.

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
High-? alteration and/or metamorphism
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Type Occurrence of RibbeiteHide

General Appearance of Type Material:
Fine-grained, anhedral granular aggregates of crystals approximately 0.5 mm in diameter with a typical granulitic texture.
Place of Conservation of Type Material:
National Museum of Natural History, Washington, D.C., USA, 163208.
Geological Setting of Type Material:
Ribbeite occurs as pinkish lenses up to 5 cm thick and 20 cm long within a 20-m-wide zone of tectonically intercalated manganese and iron ores. Locally within the stope environs, the complexly deformed manganese andiron ores assume the attitude of a vertically plunging cylindroidal fold in which ribbeite has a preferential association with carbonate-silicate facies within the manganese ores. The lenses are derived by tectonic transposition and boudinaging of the original sedimentary protore layering. The area containing ribbeite measured only ca. 40 cm across as exposed on the stope back. Ribbeite can be regarded as a scarce mineral. The transposed layering is transgressed by an abundance of veinlets of a proposed new manganese hydroxy-carbonate that clearly postdate the major tectonism but are themselves slightly deformed. Of interest also is the occurrence of manganosite as a constituent (to 5olo by volume) of some hausmannite-pyrochroite-barite-calcite layers within the Mn ores but not immediately associated with the ribbeite-alleghanyite layers. The manganosite is altering to pyrochroite and hausmannite and occurs as ragged emerald-green relicts up to 2 cm in diameter. The textural evidence strongly suggests that manganosite was a syngenetic precursor of the hausmannite ores.
Associated Minerals at Type Locality:

Synonyms of RibbeiteHide

Other Language Names for RibbeiteHide

Dutch:Ribbeiet
German:Ribbeit
Spanish:Ribbeita

Relationship of Ribbeite to other SpeciesHide

Other Members of Leucophoenicite Subgroup:
JerrygibbsiteMn2+9(SiO4)4(OH)2Orth. mmm(2/m2/m2/m) : Pbcn
LeucophoeniciteMn2+7(SiO4)3(OH)2Mon. 2/m : P21/b

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Ribbeite associated with HausmanniteMn2+Mn3+2O4

Related Minerals - Strunz-mindat GroupingHide

9.AF.ChegemiteCa7(SiO4)3(OH)2Orth. mmm(2/m2/m2/m)
9.AF.Jingwenite-(Y)YAlV4+(SiO4)O2(OH)2Mon. 2/m
9.AF.BarwooditeMn2+6Nb5+(SiO4)2O3(OH)3Trig. 3 : P3
9.AF.05SillimaniteAl2(SiO4)OOrth. mmm(2/m2/m2/m)
9.AF.05'Xenolite'Al10Si8O31
9.AF.10KanonaiteMn3+Al(SiO4)OOrth. mmm(2/m2/m2/m) : Pnnm
9.AF.10AndalusiteAl2(SiO4)OOrth. mmm(2/m2/m2/m) : Pnnm
9.AF.15KyaniteAl2(SiO4)OTric. 1 : P1
9.AF.20KrieseliteAl2(GeO4)F2Orth. mmm(2/m2/m2/m) : Pnma
9.AF.20MulliteAl4+2xSi2-2xO10-xOrth. mmm(2/m2/m2/m) : Pbam
9.AF.23BoromulliteAl9BSi2O19Orth. mm2 : Cmc21
9.AF.25YoderiteMg(Al,Fe3+)3(SiO4)2O(OH)Mon. 2/m : P21/m
9.AF.30ZincostauroliteZn2Al9Si4O23(OH)Mon. 2/m : B2/m
9.AF.30StauroliteFe2+2Al9Si4O23(OH)Mon. 2/m : B2/m
9.AF.30MagnesiostauroliteMg(Mg,Li)3(Al,Mg)18Si8O44(OH)4Mon. 2/m : B2/m
9.AF.35TopazAl2(SiO4)(F,OH)2Orth. mmm(2/m2/m2/m)
9.AF.40NorbergiteMg3(SiO4)F2Orth. mmm(2/m2/m2/m)
9.AF.45ChondroditeMg5(SiO4)2F2Mon. 2/m : P21/b
9.AF.45KumtyubeiteCa5(SiO4)2F2Mon. 2/m : P21/b
9.AF.45ReinhardbraunsiteCa5(SiO4)2(OH,F)2Mon. 2/m : P21/b
9.AF.45HydroxylchondroditeMg5(SiO4)2(OH)2Mon. 2/m : P21/b
9.AF.45AlleghanyiteMn2+5(SiO4)2(OH)2Mon. 2/m : P21/b
9.AF.50'Unnamed (Ca-analogue of Humite)'Ca7(SiO4)4F2Orth. mmm(2/m2/m2/m)
9.AF.50HumiteMg7(SiO4)3F2Orth. mmm(2/m2/m2/m) : Pnma
9.AF.50ManganhumiteMn2+7(SiO4)3(OH)2Orth. mmm(2/m2/m2/m)
9.AF.50'Unnamed (OH-analogue of humite)'Mg7(SiO4)3(OH)2Orth.
9.AF.50FluorchegemiteCa7(SiO4)3F2 Orth. mmm(2/m2/m2/m)
9.AF.55HydroxylclinohumiteMg9(SiO4)4(OH)2Mon. 2/m : P21/b
9.AF.55ClinohumiteMg9(SiO4)4F2Mon. 2/m : P21/b
9.AF.55SonoliteMn2+9(SiO4)4(OH)2Mon. 2/m : P21/b
9.AF.60LeucophoeniciteMn2+7(SiO4)3(OH)2Mon. 2/m : P21/b
9.AF.70JerrygibbsiteMn2+9(SiO4)4(OH)2Orth. mmm(2/m2/m2/m) : Pbcn
9.AF.75FranciscaniteMn2+6(V5+,◻)2(SiO4)2(O,OH)6Trig. 3 : P3
9.AF.75ScorticoiteMn6(Sb,◻)Σ2(SiO4)2O3(OH)3Trig. 3 : P3
9.AF.75WeliniteMn2+6(W6+,Mg)2(SiO4)2(O,OH)6Trig. 3 : P3
9.AF.75ÖrebroiteMn2+3(Sb5+,Fe3+)(SiO4)(O,OH)3Trig. 3 : P3
9.AF.80EllenbergeriteMg6(Mg,Ti,Zr,◻)2(Al,Mg)6Si8O28(OH)10Hex. 6 : P63
9.AF.85MagnesiochloritoidMgAl2O(SiO4)(OH)2Mon. 2/m : B2/b
9.AF.85OttréliteMn2+Al2O(SiO4)(OH)2Mon.
9.AF.85ChloritoidFe2+Al2O(SiO4)(OH)2Mon. 2/m : B2/b
9.AF.90OlmiiteCaMn2+[SiO3(OH)](OH)Orth. mmm(2/m2/m2/m) : Pbca
9.AF.90PoldervaartiteCaCa[SiO3(OH)](OH)Orth. mmm(2/m2/m2/m) : Pbca
9.AF.95Pilawite-(Y)Ca2Y2Al4(SiO4)4O2(OH)2Mon. 2/m : P21/b

Fluorescence of RibbeiteHide

Not fluorescent in UV

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 RibbeiteHide

References for RibbeiteHide

Localities for RibbeiteHide

Showing 16 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.
Japan
 
  • Ehime Prefecture
    • Ouzu City
      • Nagahama
Minakawa et al (1991)
  • Gifu Prefecture
    • Mino City
Masutomi Museum specimen (Kyoto)
  • Nagano Prefecture
    • Kamiina District
      • Hamayokokawa mine (Hamayokogawa mine)
Akira Kato (2011)
  • Shiga Prefecture
    • Takashima City
Masutomi Museum specimen (Kyoto)
Yamada (2004)
Yamada (2004)
  • Tochigi Prefecture
    • Kanuma City
Akira Kato (undated manuscript) +1 other reference
Namibia (TL)
 
  • Otjozondjupa Region
    • Otavi Constituency
      • Kombat
Peacor et al. (1987) +2 other references
Romania
 
Hîrtopanu et al. (2003) +1 other reference
  • Maramureș County
    • Târgu Lăpuș
minerals-of-the-carpathians.eu (2008) +2 other references
  • Suceava County
    • Iacobeni
      • Tolovanu
Hîrtopanu (1997) +1 other reference
Russia
 
  • Bashkortostan
    • Sibay
Brusnitsyn et al. (2002) +1 other reference
  • Komi Republic
Brusnitsyn +1 other reference
Spain
 
  • Canary Islands
    • Santa Cruz de Tenerife Province
      • Tenerife
        • Granadilla de Abona
Dill et al. (2023)
Switzerland
 
  • Valais
    • Leuk
      • Turtmann-Unterems
        • Turtmann Valley
          • Pipjitälli
The Canadian Mineralogist Vol. 44 (2006)
USA
 
  • New Jersey
    • Sussex County
      • Franklin
Heixhong Yang
 
and/or  
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