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Fluorphosphohedyphane
A valid IMA mineral species
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About Fluorphosphohedyphane
Formula:
Ca2Pb3(PO4)3F
Colour:
Colourless
Lustre:
Sub-Adamantine
Hardness:
4
Specific Gravity:
5.445 (Calculated)
Crystal System:
Hexagonal
Member of:
Name:
Named for being the fluorine-analogue of phosphohedyphane.
Unique Identifiers
Mindat ID:
39334
Long-form identifier:
mindat:1:1:39334:0
IMA Classification of Fluorphosphohedyphane
Classification of Fluorphosphohedyphane
8.BN.05
8 : PHOSPHATES, ARSENATES, VANADATES
B : Phosphates, etc., with additional anions, without H2O
N : With only large cations, (OH, etc.):RO4 = 0.33:1
8 : PHOSPHATES, ARSENATES, VANADATES
B : Phosphates, etc., with additional anions, without H2O
N : With only large cations, (OH, etc.):RO4 = 0.33:1
41.8.4.3
41 : ANHYDROUS PHOSPHATES, ETC.CONTAINING HYDROXYL OR HALOGEN
8 : A5(XO4)3Zq
41 : ANHYDROUS PHOSPHATES, ETC.CONTAINING HYDROXYL OR HALOGEN
8 : A5(XO4)3Zq
Mineral Symbols
As of 2021 there are now IMAâCNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
| Symbol | Source | Reference for Standard |
|---|---|---|
| Fphdy | IMAâCNMNC | Warr, L.N. (2021). IMAâCNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Fluorphosphohedyphane
Sub-Adamantine
Transparency:
Transparent
Colour:
Colourless
Streak:
White
Hardness:
4 on Mohs scale
Tenacity:
Brittle
Cleavage:
None Observed
Parting:
None observed
Fracture:
Sub-Conchoidal
Density:
5.445 g/cm3 (Calculated)
Optical Data of Fluorphosphohedyphane
Type:
Uniaxial (-)
RI values:
nω = 1.836(5) nε = 1.824(5)
Max. Birefringence:
δ = 0.012
Based on recorded range of RI values above.
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 Âĩm 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.
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 Âĩm 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).
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.
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:
Non-pleochroic
Chemistry of Fluorphosphohedyphane
Mindat Formula:
Ca2Pb3(PO4)3F
Element Weights:
Crystallography of Fluorphosphohedyphane
Crystal System:
Hexagonal
Class (H-M):
6/m - Dipyramidal
Space Group:
P63/m
Cell Parameters:
a = 9.6402(12) Å, c = 7.0121(8) Å
Ratio:
a:c = 1 : 0.727
Unit Cell V:
564.4 Ã
Âģ
Z:
2
Morphology:
Hexagonal prisms with pyramidal terminations. Forms observed are {100} and {101}.
Crystal Structure
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Data courtesy of the American Mineralogist Crystal Structure Database. Click on an AMCSD ID to view structure
| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0018322 | Fluorphosphohedyphane | Kampf A R, Housley R M (2011) Fluorphosphohedyphane, Ca2Pb3(PO4)3F, the first apatite supergroup mineral with essential Pb and F American Mineralogist 96 423-429 | 2011 | Blue Bell claims, near Baker, San Bernardino County, California, USA | 0 | 293 | |
| 0013569 | Fluorphosphohedyphane | Miyake M, Ishigaki K, Suzuki T (1986) Structure refinements of Pb2+ ion-exchanged apatites by X-ray powder pattern-fitting Journal of Solid State Chemistry 61 230-235 | 1986 | synthetic | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 8.384 Ã | (20) |
| 3.978 Ã | (26) |
| 3.509 Ã | (23) |
| 3.239 Ã | (12) |
| 3.161 Ã | (15) |
| 2.8805 Ã | (100) |
| 2.3485 Ã | (17) |
| 2.0981 Ã | (20) |
| 1.9332 Ã | (13) |
| 1.8792 Ã | (26) |
| 1.8488 Ã | (12) |
| 1.7930 Ã | (13) |
| 1.5664 Ã | (10) |
| 1.4820 Ã | (10) |
| 1.2814 Ã | (13) |
| 1.2630 Ã | (10) |
Comments:
Blue Bell Mine, San Bernardino Co., California, USA. Data from the type description.
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 7: Great Oxidation Event | <2.4 |
| 47c : [Carbonates, phosphates, borates, nitrates] | |
| 47g : [Halogen-bearing surface weathering minerals] |
Type Occurrence of Fluorphosphohedyphane
General Appearance of Type Material:
Hexagonal prisms with pyramidal terminations up to about 0.5 mm in length; in sub-parallel intergrowths and irregular clusters.
Place of Conservation of Type Material:
Natural History Museum of Los Angeles County under catalog numbers 60550, 60551, 60552, 60553, 60554, and 60555.
Geological Setting of Type Material:
In cracks and narrow veins in a highly siliceous quartzite-like hornfels in a fractured and chaotic region of limestone showing irregular skarn formation.
Associated Minerals at Type Locality:
Synonyms of Fluorphosphohedyphane
Other Language Names for Fluorphosphohedyphane
Relationship of Fluorphosphohedyphane to other Species
Member of:
Other Members of Hedyphane Group:
| Aiolosite | Na4Bi(SO4)3Cl | Hex. 6/m : P63/m |
| Caracolite | Na3Pb2(SO4)3Cl | Mon. 2/m : P21/m |
| Cesanite | Na3Ca2(SO4)3(OH) | Hex. 6 : P6 |
| Fluorsigaiite | Ca2Sr3(PO4)3F | Hex. 6/m : P63/m |
| Hedyphane | Ca2Pb3(AsO4)3Cl | Hex. 6/mmm(6/m2/m2/m) : P63/mmc |
| Hydroxylhedyphane | Ca2Pb3(AsO4)3(OH) | Trig. 3 : P3 |
| Miyahisaite | (Sr,Ca)2Ba3(PO4)3F | Hex. 6/m : P63/m |
| Morelandite | Ca2Ba3(AsO4)3Cl | Hex. |
| Parafiniukite | Ca2Mn3(PO4)3Cl | Hex. 6/m : P63/m |
| Phosphohedyphane | Ca2Pb3(PO4)3Cl | Hex. 6/m : P63/m |
| 'UM2002-53-PO:CaHPb' | Ca2Pb3(PO4)3(OH,Cl,F) |
Common Associates
Associations Based on Photo Data:
| 7 photos of Fluorphosphohedyphane associated with Pyromorphite | Pb5(PO4)3Cl |
| 4 photos of Fluorphosphohedyphane associated with Opal | SiO2 · nH2O |
| 4 photos of Fluorphosphohedyphane associated with Wulfenite | Pb(MoO4) |
| 4 photos of Fluorphosphohedyphane associated with Reynoldsite | Pb2Mn4+2O5(CrO4) |
| 2 photos of Fluorphosphohedyphane associated with Hemimorphite | Zn4Si2O7(OH)2 · H2O |
| 2 photos of Fluorphosphohedyphane associated with Quartz | SiO2 |
| 2 photos of Fluorphosphohedyphane associated with 'Limonite' |
Related Minerals - Strunz-mindat Grouping
| 8.BN. | Fluoralforsite | Ba5(PO4)3F |
| 8.BN. | Aradite | BaCa6[(SiO4)(VO4)](VO4)2F |
| 8.BN. | Magganasite | CuFe3+3O(AsO4)3 |
| 8.BN. | Fluorpyromorphite | Pb5(PO4)3F |
| 8.BN. | Fluorsigaiite | Ca2Sr3(PO4)3F |
| 8.BN.05 | Pieczkaite | Mn5(PO4)3Cl |
| 8.BN.05 | Fluorapatite | Ca5(PO4)3F |
| 8.BN.05 | Fluorcaphite | SrCaCa3(PO4)3F |
| 8.BN.05 | Vanadinite | Pb5(VO4)3Cl |
| 8.BN.05 | Hedyphane | Ca2Pb3(AsO4)3Cl |
| 8.BN.05 | Hydroxylhedyphane | Ca2Pb3(AsO4)3(OH) |
| 8.BN.05 | 'Mimetite-M' | Pb5(AsO4)3Cl |
| 8.BN.05 | Johnbaumite | Ca5(AsO4)3(OH) |
| 8.BN.05 | Pliniusite | Ca5(VO4)3F |
| 8.BN.05 | 'Hydroxylapatite-M' | Ca5(PO4)3OH |
| 8.BN.05 | Hydroxylpyromorphite | Pb5(PO4)3(OH) |
| 8.BN.05 | Miyahisaite | (Sr,Ca)2Ba3(PO4)3F |
| 8.BN.05 | Carlgieseckeite-(Nd) | NaNdCa3(PO4)3F |
| 8.BN.05 | Belovite-(Ce) | NaCeSr3(PO4)3F |
| 8.BN.05 | Kuannersuite-(Ce) | NaCeBa3(PO4)3F0.5Cl0.5 |
| 8.BN.05 | Alforsite | Ba5(PO4)3Cl |
| 8.BN.05 | 'Unnamed (OH-analogue of Mimetite)' | Pb5(AsO4)3(OH) |
| 8.BN.05 | Stronadelphite | Sr5(PO4)3F |
| 8.BN.05 | Parafiniukite | Ca2Mn3(PO4)3Cl |
| 8.BN.05 | Mimetite | Pb5(AsO4)3Cl |
| 8.BN.05 va | 'Germanate-pyromorphite' | Pb5(PO4)2GeO4 |
| 8.BN.05 | Belovite-(La) | NaLaSr3(PO4)3F |
| 8.BN.05 | Fluorstrophite | SrCaSr3(PO4)3F |
| 8.BN.05 | Hydroxylapatite | Ca5(PO4)3(OH) |
| 8.BN.05 | 'Johnbaumite-M' | Ca5(AsO4)3OH |
| 8.BN.05 | Phosphohedyphane | Ca2Pb3(PO4)3Cl |
| 8.BN.05 | Turneaureite | Ca5(AsO4)3Cl |
| 8.BN.05 | Morelandite | Ca2Ba3(AsO4)3Cl |
| 8.BN.05 | 'Oxypyromorphite' | Pb10(PO4)6O |
| 8.BN.05 | Deloneite | (Na0.5REE0.25Ca0.25)(Ca0.75REE0.25)Sr1.5(CaNa0.25REE0.25)(PO4)3F0.5(OH)0.5 |
| 8.BN.05 | Chlorapatite | Ca5(PO4)3Cl |
| 8.BN.05 | Pyromorphite | Pb5(PO4)3Cl |
| 8.BN.05 | Vanackerite | Pb4Cd(AsO4)3Cl |
| 8.BN.05 | Svabite | Ca5(AsO4)3F |
| 8.BN.10 | Arctite | Na2Ca4(PO4)3F |
| 8.BN.10 | KrÞgerite | BaCa6(SiO4)2[(P0.5S0.5)O4]2F |
| 8.BN.15 | Goryainovite | Ca2(PO4)Cl |
Fluorescence of Fluorphosphohedyphane
Non-fluorescent.
Other Information
Notes:
Decomposed quickly in HCl and the residue dissolves slowly.
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 Fluorphosphohedyphane
mindat.org URL:
https://www.mindat.org/min-39334.html
Please feel free to link to this page.
Please feel free to link to this page.
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References for Fluorphosphohedyphane
Reference List:
Pasero, Marco, Kampf, Anthony R., Ferraris, Cristiano, Pekov, Igor V., Rakovan, John, White, Timothy J. (2010) Nomenclature of the apatite supergroup minerals. European Journal of Mineralogy, 22 (2) 163-179 doi:10.1127/0935-1221/2010/0022-2022
Localities for Fluorphosphohedyphane
Showing 10 localities.
Locality List
- This locality has map coordinates listed.
- This locality has estimated coordinates.
â - 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).
All localities listed without proper references should be considered as questionable.
Austria | |
| Knobloch et al. (2018) |
China | |
| Gui-jun Zhu (2022) |
Germany | |
| Markl et al. (2014) |
| MÃķhn et al. (12/2023) |
| Markl et al. (2014) |
| Witzke (2024) |
Norway | |
| Folvik (2019) |
Russia | |
| Pekov et al. (2025) +1 other reference |
USA (TL) | |
| Kampf et al. (2011) +1 other reference |
| In the collection of Alex Earl |
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The
Blue Bell Mine, Zzyzx, Soda Mountains, Silver Lake Mining District, San Bernardino County, California, USA