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Parafransoletite

A valid IMA mineral species
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About ParafransoletiteHide

Formula:
Ca3Be2(PO4)2(PO3OH)2 · 4H2O
Colour:
Colorless, white
Lustre:
Vitreous, Silky
Hardness:
Specific Gravity:
2.54
Crystal System:
Triclinic
Name:
Named for its dimorphous relationship with fransoletite.
This page provides mineralogical data about Parafransoletite.


Unique IdentifiersHide

Mindat ID:
3089
Long-form identifier:
mindat:1:1:3089:8

IMA Classification of ParafransoletiteHide

Approved
IMA Formula:
Ca3Be2(PO4)2(PO3OH)2·4H2O
Approval year:
1989
First published:
1992

Classification of ParafransoletiteHide

8.CA.05

8 : PHOSPHATES, ARSENATES, VANADATES
C : Phosphates without additional anions, with H2O
A : With small and large/medium cations
Dana 7th ed.:
40.5.2.1
40.5.2.1

40 : HYDRATED NORMAL PHOSPHATES,ARSENATES AND VANADATES
5 : AXO4·xH2O

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

Physical Properties of ParafransoletiteHide

Vitreous, Silky
Transparency:
Transparent, Translucent
Colour:
Colorless, white
Streak:
White
Hardness:
2½ on Mohs scale
Tenacity:
Brittle
Cleavage:
None Observed
Comment:
'Even' fracture.
Density:
2.54(1) g/cm3 (Measured)    2.27 g/cm3 (Calculated)

Optical Data of ParafransoletiteHide

Type:
Biaxial (+)
RI values:
nα = 1.562 nβ = 1.564 nγ = 1.588
2V:
Measured: 33° , Calculated: 34°
Max. Birefringence:
δ = 0.026
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:
strong
Optical Extinction:
θ = 85°; ψ = –13°; φ = 98°.

Chemistry of ParafransoletiteHide

Mindat Formula:
Ca3Be2(PO4)2(PO3OH)2 · 4H2O
Element Weights:
Element% weight
O54.032 %
P20.920 %
Ca20.302 %
Be3.044 %
H1.702 %

Calculated from ideal end-member formula.

Crystallography of ParafransoletiteHide

Crystal System:
Triclinic
Class (H-M):
1 - Pinacoidal
Space Group:
P1
Cell Parameters:
a = 7.32 Å, b = 7.69 Å, c = 7.06 Å
α = 94.9°, β = 96.82°, γ = 101.86°
Ratio:
a:b:c = 0.952 : 1 : 0.918
Unit Cell V:
385.48 ų
Z:
1
Morphology:
Thin individual spear-shaped blades, sheaf- and bowtie-like aggregates, and compact radial sprays. Similar to collinsite in appearance and notably distinct from fransoletite. Most crystals are composite with slightly rounded faces tapering to a pointed termination. Individual crystals are flattened on {010} and elongate parallel to [100]. Forms include {010}, {011}, {131}, {131}, and {144}. Doubly terminated crystals are common and seemingly exhibit centrosymmetric development of crystal forms.
Twinning:
Simple contact twinning on {010} is common.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0001532ParafransoletiteKampf A R (1992) Beryllophosphate chains in the structures of fransoletite, parafransoletite, and ehrleite and some general comments on beryllophosphate linkages American Mineralogist 77 848-85619920293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.032 Å(100)
3.619 Å(80)
2.595 Å(60)
7.52 Å(50)
2.334 Å(40)
2.485 Å(25)
1.870 Å(25)
Comments:
Tip Top mine, South Dakota, USA. The data are from the type description.

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
22 : Hydration and low-? subsurface aqueous alteration (see also #23)

Type Occurrence of ParafransoletiteHide

General Appearance of Type Material:
Thin individual spear-shaped blades up to 0.4 x 0.1 x 0.04 mm, as sheaf- and bowtie-like aggregates, and as compact radial sprays to 2 mm in diameter. It is similar to collinsite in appearance and notably distinct from fransoletite.
Place of Conservation of Type Material:
Natural History Museum, Los Angeles, California, USA, number 35696.
National Museum of Natural History, Washington, D.C., USA, number 168432.
Geological Setting of Type Material:
Granite pegmatite.
Associated Minerals at Type Locality:

Synonyms of ParafransoletiteHide

Other Language Names for ParafransoletiteHide

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Parafransoletite associated with MontgomeryiteCa4MgAl4(PO4)6(OH)4 · 12H2O
1 photo of Parafransoletite associated with RobertsiteCa2Mn3+3(PO4)3O2 · 3H2O

Related Minerals - Strunz-mindat GroupingHide

8.CA.ApexiteNaMg(PO4) · 9H2OTric. 1 : P1
8.CA.BrandãoiteBeAl2(PO4)2(OH)2(H2O)5Tric. 1 : P1
8.CA.DavidlloyditeZn3(AsO4)2 · 4H2OTric. 1 : P1
8.CA.05FransoletiteCa3Be2(PO4)2(PO3OH)2 · 4H2OMon. 2/m : P21/b
8.CA.10EhrleiteCa4Be3Zn2(PO4)6 · 9H2OTric. 1 : P1
8.CA.15FaheyiteBe2Mn2+Fe3+2(PO4)4 · 6H2OTrig. 32 : P3121
8.CA.20MccrillisiteNaCs(Be,Li)Zr2(PO4)4 · 1-2H2OTet. 4/mmm(4/m2/m2/m) : I41/amd
8.CA.20GainesiteNa(Na,K)(Be,Li)Zr2(PO4)4 · 1.5-2H2OTet. 4mm : I41md
8.CA.20SelwyniteNaK(Be,Al)Zr2(PO4)4 · 2H2OTet. 4/mmm(4/m2/m2/m) : I41/amd
8.CA.25PahasapaiteLi8(Ca,Li,K)10.5Be24(PO4)24 · 38H2OIso. 23 : I23
8.CA.30NizamoffiteMn2+Zn2(PO4)2(H2O)4Orth. mmm(2/m2/m2/m) : Pbcm
8.CA.30ArsenohopeiteZn3(AsO4)2 · 4H2OOrth. mmm(2/m2/m2/m) : Pnma
8.CA.30HopeiteZnZn2(PO4)2 · 4H2OOrth. mmm(2/m2/m2/m) : Pnma
8.CA.35WarikahniteZn3(AsO4)2 · 2H2OTric. 1 : P1
8.CA.40PhosphophylliteZn2Fe 2+(PO4)2 · 4H2OMon. 2/m : P21/b
8.CA.42SteinmetziteZn2Fe3+(PO4)2(OH) · 3H2OTric. 1 : P1
8.CA.45ParascholziteCaZn2(PO4)2 · 2H2OMon.
8.CA.45ScholziteCaZn2(PO4)2 · 2H2OOrth. mmm(2/m2/m2/m) : Pbcm
8.CA.50KeyiteCu2+3Zn4Cd2(AsO4)6 · 2H2OMon. 2/m
8.CA.55PushcharovskiteK0.6Cu18[AsO2(OH)2]4[AsO3OH]10(AsO4)(OH)9.6 · 18.6H2OTric.
8.CA.60ProsperiteCa2Zn4(AsO4)4 · H2OMon.
8.CA.65GengenbachiteKFe3+3(PO3OH)4[PO2(OH)2]2 · 6H2OTrig. 3m : P31c
8.CA.70ParahopeiteZn3(PO4)2 · 4H2OTric. 1 : P1
8.CA.70ReaphookhilliteMgZn2(PO4)2 · 4H2OTric. 1 : P1
8.CA.75StergiouiteCaZn2(AsO4)2 · 4H2OMon. m : Pb
8.CA.80LimousiniteBaCa[Be4P4O16] · 6H2OMon. 2/m : P21/b
8.CA.85MinjiangiteBaBe2(PO4)2Hex. 6/mmm(6/m2/m2/m) : P6/mmm
8.CA.85Wilancookite(Ba5Li2◻)Ba6Be24P24O96 · 26H2OIso. 23 : I23

Fluorescence of ParafransoletiteHide

Not fluorescent.

Other InformationHide

Notes:
Dissolves readily in cold 1:1 HCl.
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 ParafransoletiteHide

References for ParafransoletiteHide

Localities for ParafransoletiteHide

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.
USA (TL)
 
  • South Dakota
    • Custer County
      • Custer Mining District
        • Fourmile
Kampf et al. (1992)
 
and/or  
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