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Ellenbergerite

A valid IMA mineral species
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About EllenbergeriteHide

05157710017271922704552.jpg
François T. V. Ellenberger
Formula:
Mg6(Mg,Ti,Zr,◻)2(Al,Mg)6Si8O28(OH)10
Colour:
Purple to lilac; some individuals exhibit smoky or pink cores.
Lustre:
Vitreous
Hardness:
Specific Gravity:
3.15 - 3.22
Crystal System:
Hexagonal
Name:
Named by Chopin et al. in 1986 in honor of François Théodore Victor Ellenberger (5 May 1915, Lealui, Northern Rhodesia (now Zambia) - 11 January 2000, Bures-sur-Yvette, France), Professor of Structural Geology, University of the Sorbonne, Paris, for his work in the western Alps. In 1976 he created the French Committee of History of Geology (COFRHIGEO) and published 'Histoire de la Géologie' in two volumes (1988 and 1994).
The Type Locality is indicated as Case Parigi (better Case Paris as known "in loco") but the classic outcrop is very near to Case Ramello.

Closely related to phosphoellenbergerite. Compare 'ellenbergerite-(PO4)'.


Unique IdentifiersHide

Mindat ID:
1366
Long-form identifier:
mindat:1:1:1366:2

Similar NamesHide

Ellenbergerite-(PO4)(Mg,◻)2(Mg,Al)12(SiO3OH)6(PO3OH)(OH)6

IMA Classification of EllenbergeriteHide

Classification of EllenbergeriteHide

9.AF.80

9 : SILICATES (Germanates)
A : Nesosilicates
F : Nesosilicates with additional anions; cations in [4], [5] and/or only [6] coordination
52.4.10.1

52 : NESOSILICATES Insular SiO4 Groups and O,OH,F,H2O
4 : Insular SiO4 Groups and O, OH, F, and H2O with cations in [6] and/or >[6] coordination
16.14.10

16 : Silicates Containing Aluminum and other Metals
14 : Aluminosilicates of Ti, Zr, Sn and Pb

Mineral SymbolsHide

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

Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.

SymbolSourceReference for Standard
EllIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43
EllWhitney & Evans (2010)Whitney, D.L. and Evans, B.W. (2010) Abbreviations for names of rock-forming minerals. American Mineralogist, 95, 185–187 doi:10.2138/am.2010.3371
EllThe Canadian Mineralogist (2019)The Canadian Mineralogist (2019) The Canadian Mineralogist list of symbols for rock- and ore-forming minerals (December 30, 2019). download

Pronunciation of EllenbergeriteHide

Pronunciation:
PlayRecorded byCountry
Jolyon RalphUnited Kingdom

Physical Properties of EllenbergeriteHide

Vitreous
Transparency:
Transparent
Colour:
Purple to lilac; some individuals exhibit smoky or pink cores.
Hardness:
6½ on Mohs scale
Tenacity:
Brittle
Density:
3.15 - 3.22 g/cm3 (Measured)    3.13(4) g/cm3 (Calculated)

Optical Data of EllenbergeriteHide

Type:
Uniaxial (-)
RI values:
nω = 1.6553 - 1.6789 nε = 1.6538 - 1.6697
Max. Birefringence:
δ = 0.002 - 0.009
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 uniaxial interference figure - the conoscopic (convergent-light, Bertrand-lens-in) view, for a grain cut with the optic axis centred and vertical. The coloured rings are isochromatics, computed with the same physics as the Michel-Lévy bar above; the dark cross is the isogyre.

For a genuinely uniaxial mineral viewed this way, that cross stays perfectly stationary if you rotate the stage - unlike a biaxial mineral, where it splits apart on rotation. That invariance is itself the standard diagnostic test for telling uniaxial and biaxial minerals apart at the microscope.
Pleochroism:
Strong
Comments:
O = colorless; E = colorless to deep lilac

Chemistry of EllenbergeriteHide

Mindat Formula:
Mg6(Mg,Ti,Zr,◻)2(Al,Mg)6Si8O28(OH)10
Element Weights:
Element% weight
O50.704 %
Si18.738 %
Mg16.216 %
Al13.501 %
H0.841 %

Calculated from ideal end-member formula.
O
Si
Mg
Al
H
Common Impurities:
Zr,Fe,P

Chemical AnalysisHide

Oxide wt%:
 12
SiO231.19 %39.29 %
P2O511.32 %0.69 %
TiO20.34 %2.36 %
ZrO21.44 %
Al2O319.00 %24.28 %
FeO0.50 %0.50 %
MnO0.03 %0.06 %
MgO27.16 %22.12 %
CaO0.06 %0.02 %
Na2O0.00 %0.00 %
K2O0.01 %0.00 %
Total:89.61 %90.76 %
Sample references:
IDLocalityReferenceNotes
1Case Parigi, Martiniana Po, Cuneo Province, Piedmont, ItalySample taken from an inclusion in the inner portion of a pyrope megacryst from a coesite-phengite-pyrope whiteschist. The sample is intermediate in composition between ellenbergerite and phosphoellenbergerite. Mineral analyses were performed by means of the Cameca electron microprobe (CAMEBAX) , using a wavelength-dispersive technique with PAP correction acceleration voltage 15 kV, beam current 15 nA, measuring time 20 s).
2  "  "Sample taken from an inclusion in the outer portion of a pyrope megacryst from a coesite-phengite-pyrope whiteschist. Mineral analyses were performed by means of the Cameca electron microprobe (CAMEBAX) , using a wavelength-dispersive technique with PAP correction acceleration voltage 15 kV, beam current 15 nA, measuring time 20 s).

Crystallography of EllenbergeriteHide

Crystal System:
Hexagonal
Class (H-M):
6 - Pyramidal
Space Group:
P63
Cell Parameters:
a = 12.255(8) Å, c = 4.932(4) Å
Ratio:
a:c = 1 : 0.402
Unit Cell V:
641.48 ų (Calculated from Unit Cell)
Z:
1

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0006485EllenbergeriteComodi P, Zanazzi P F (1993) Structural study of ellenbergerite. Part 1: Effects of high temperature European Journal of Mineralogy 5 819-82919930293
0006484EllenbergeriteComodi P, Zanazzi P F (1993) Structural study of ellenbergerite. Part 1: Effects of high temperature European Journal of Mineralogy 5 819-82919930293
0006486EllenbergeriteComodi P, Zanazzi P F (1993) Structural study of ellenbergerite. Part 1: Effects of high temperature European Journal of Mineralogy 5 819-82919930683
0006487EllenbergeriteComodi P, Zanazzi P F (1993) Structural study of ellenbergerite. Part 1: Effects of high temperature European Journal of Mineralogy 5 819-82919930941
0006488EllenbergeriteComodi P, Zanazzi P F (1993) Structural study of ellenbergerite. Part II: Effects of high pressure European Journal of Mineralogy 5 831-83819930.4293
0006489EllenbergeriteComodi P, Zanazzi P F (1993) Structural study of ellenbergerite. Part II: Effects of high pressure European Journal of Mineralogy 5 831-83819933.2293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.11 Å(100)
3.54 Å(75)
2.653 Å(70)
3.06 Å(55)
2.183 Å(55)
3.61 Å(50)
2.337 Å(30)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 5: Initiation of plate tectonics<3.5-2.5
39 : High-? metamorphism (blueschist, eclogite, ultrahigh ? facies)

Type Occurrence of EllenbergeriteHide

General Appearance of Type Material:
Anhedral inclusions in pyrope crystals.
Place of Conservation of Type Material:
University of Pierre and Marie Curie, Paris; National School of Mines, Paris, France; Institute for Mineralogy, Ruhr University, Bochum, Germany; National Museum of Natural History, Washington, D.C., USA, 163497.
Geological Setting of Type Material:
As inclusions in pyrope porphyroblasts developed during high-pressure (25-30 kbar), medium-temperature (700±C - 800±C) metamorphism of continental crustal rocks.
Associated Minerals at Type Locality:

Synonyms of EllenbergeriteHide

Other Language Names for EllenbergeriteHide

Common AssociatesHide

Associations Based on Photo Data:
6 photos of Ellenbergerite associated with RutileTiO2
5 photos of Ellenbergerite associated with PyropeMg3Al2(SiO4)3
3 photos of Ellenbergerite associated with MagnesiostauroliteMg(Mg,Li)3(Al,Mg)18Si8O44(OH)4
1 photo of Ellenbergerite associated with KyaniteAl2(SiO4)O
1 photo of Ellenbergerite associated with CoesiteSiO2
1 photo of Ellenbergerite associated with MuscoviteKAl2(AlSi3O10)(OH)2

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.65RibbeiteMn2+5(SiO4)2(OH)2Orth. mmm(2/m2/m2/m)
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.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

Other InformationHide

Notes:
Faint blue cathodoluminescence.
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 EllenbergeriteHide

References for EllenbergeriteHide

Reference List:

Localities for EllenbergeriteHide

Showing 3 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.
Italy
 
  • Piedmont
    • Cuneo Province
      • Brossasco
Simon et al. (2001)
Chopin et al. (1986) +1 other reference
      • Martiniana Po
Chopin et al. (1986) +2 other references
 
and/or  
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