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Fluocerite-(La)

A valid IMA mineral species
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About Fluocerite-(La)Hide

Formula:
LaF3
Hardness:
4 - 5
Crystal System:
Trigonal
Name:
In allusion to its relationship to Fluocerite-(Ce), plus the "-(La)" suffix due to the dominance of lanthanum in the composition.
The lanthanum analogue of Fluocerite-(Ce).


Unique IdentifiersHide

Mindat ID:
1568
Long-form identifier:
mindat:1:1:1568:0

Similar NamesHide

FluoceriteA synonym
Fluocerite-(Ce)A valid IMA mineral species - grandfatheredCeF3
Flusscerit

IMA Classification of Fluocerite-(La)Hide

Approved
IMA Formula:
La3+F3

Classification of Fluocerite-(La)Hide

3.AC.15

3 : HALIDES
A : Simple halides, without H2O
C : M:X = 1:3
9.3.4.2

9 : NORMAL HALIDES
3 : AX3
8.7.2

8 : Halides - Fluorides, Chlorides, Bromides and Iodides; also Fluoborates and Fluosilicates
7 : Halides of the rare earth metals

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

Physical Properties of Fluocerite-(La)Hide

Hardness:
4 - 5 on Mohs scale

Optical Data of Fluocerite-(La)Hide

Type:
Uniaxial (-)
RI values:
nω = 1.609 nε = 1.603
Max. Birefringence:
δ = 0.006
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.

Surface Relief:
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.

Chemistry of Fluocerite-(La)Hide

Mindat Formula:
LaF3
Element Weights:
Element% weight
La70.906 %
F29.094 %

Calculated from ideal end-member formula.
La
F

Crystallography of Fluocerite-(La)Hide

Crystal System:
Trigonal
Class (H-M):
3m(32/m) - Hexagonal Scalenohedral
Space Group:
P3c1
Cell Parameters:
a = 7.1871(4) Å, c = 7.3501(5) Å
Ratio:
a:c = 1 : 1.023
Unit Cell V:
328.80 ÅÂģ (Calculated from Unit Cell)
Z:
6
Comment:
For synthetic material.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0020644Fluocerite-(La)Zalkin A, Templeton D H (1985) Refinement of the trigonal structure of lanthanum trifluoride with neutron diffraction data Acta Crystallographica B41 91-931985synthetic0293
0009547Fluocerite-(La)Cheetham A K, Fender B E F, Fuess H, Wright A F (1976) A powder neutron diffraction study of lanthanum and cerium trifluorides Acta Crystallographica B32 94-971976synthetic0293
0010627Fluocerite-(La)Mansmann M (1965) Die kristallstruktur von lanthantrifluorid Zeitschrift fur Kristallographie 122 375-3981965synthetic0293
0012039Fluocerite-(La)Schlyter K (1952) On the crystal structure of fluorides of the tysonite LaF3 type Arkiv for Kemi 5 73-821952Osterby, parish of Skedevi, Dalecarlia, Sweden0293
0017899Fluocerite-(La)Oftedal I (1929) Ueber die Kristallstruktur von Tysonit und einigen kuenstlich dargestellten Lanthanidenfluoriden _cod_database_code 1010983 Zeitschrift fur Physikalische Chemie 5 272-29219290293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.60 Å(4)
3.19 Å(10)
2.07 Å(6)
2.01 Å(6)
1.796 Å(5.5)
1.736 Å(4)
1.048 Å(7)

Geological EnvironmentHide

Type Occurrence of Fluocerite-(La)Hide

Synonyms of Fluocerite-(La)Hide

Fluocerite (in part)

Other Language Names for Fluocerite-(La)Hide

Related Minerals - Strunz-mindat GroupingHide

3.AC.05ZharchikhiteAlF(OH)2Mon. 2/m : P21/b
3.AC.10MolysiteFeCl3Trig. 3 : R3
3.AC.15Fluocerite-(Ce)CeF3Trig. 3m(32/m) : P3c1
3.AC.20GananiteBiF3Iso.

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 Fluocerite-(La)Hide

References for Fluocerite-(La)Hide

Reference List:

Localities for Fluocerite-(La)Hide

Showing 7 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.
China
 
  • Henan
    • Nanyang
      • Xixia County
Qu et al. (2019)
Germany
 
  • Baden-WÞrttemberg
    • Freiburg Region
      • Ortenaukreis
        • Oberwolfach
In several collections +1 other reference
Kazakhstan
 
  • Karaganda Region
    • Karkaraly
ÐĄÐ’Ð•ÐĒЛАНА Н. НЕНАÐĻЕВА (2021)
- (1984) +1 other reference
Russia
 
  • Ural Mountains
    • Southern Urals
      • Bashkir Meganticlinorium
Kovalev et al. (2023)
Sweden
 
  • VÃĪstmanland County
    • Skinnskatteberg
      • Riddarhyttan
Öhman et al. (2005)
Andersson et al. (2024)
 
and/or  
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