FLUORITE

 


Chemical formula: CaF2

Family: Halides

Status: IMA-GP

Crystal system : Isometric

Display mineral: OUI

Associated names (luminescent varieties, discredited names, synonyms, etc.): chlorophaneyttrofluoriteyttroceriteTiffany stonefluorine

 

Luminescence:

Longwave UV (365nm) colors:

                                                                     


Blue , Bluish White , Yellowish White , Pale Yellow , Yellow , Tawn , Red , Violet Pink , Green , Greenish , Violet , Greenish white , Violet blue , Yellowish ,

Intensity LW:Very Strong

Frequency LW:Very often

Midwave UV (320nm) colors:

         


Blue , Green ,

Intensity MW:Medium

Frequency MW:Often

Shortwave UV (254nm) colors:

                                                                          


Blue , White , Bluish White , Yellowish White , Pale Yellow , Yellow , Tawn , Red , Green , Greenish , Bluish Green , Violet , Greenish white , Violet blue , Yellowish ,

Intensity SW:Medium

Frequency SW:Often


Daylight picture


FLUORITE;
Blue Circle Cement Quarry, Eastgate, Weardale, North Pennines, County Durham, England, UK
Photo and Copyright:
Middleearthminerals.com
Used with permission of the author

Longwave (365nm) picture


FLUORITE;
Blue Circle Cement Quarry, Eastgate, Weardale, North Pennines, County Durham, England, UK
UVLW, Photo and Copyright:
Middleearthminerals.com
Used with permission of the author

 

Pictures Galery:

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Phosphorescence (in the common sense of the term) observable with the naked eye:

Type d'UV

Couleur

Intensité

Fréquence d'observation

UV longs (365nm):

Greenish white StrongRarely

UV moyens (320 nm):

Greenish white

UV courts (254 nm):

Greenish white StrongRarely
 

Triboluminescence: OUI

Thermoluminescence: OUI

Comments:

The classical fluorescing mineral but all fluorites are not luminescent under UV !


CHLOROPHANE variety : green thermoluminescence ;


YTTROFLUORITE variety: SW and LW : yellow, yellowish-white (cream);

 

Activator(s) and spectrum:

Activator(s): Eu2+, ST (Singlet-triplet)-Matière organique en impureté,  Sm2+,  Ce3+,  Sm3+,  Eu3+,  Dy3+,  Ho3+,  Er3+,  Tb3+,  Pr3+,  Nd3+,  Yb3+,  Tm3+,  

Peaks in the spectrum (nm):

Eu2+ repl. Ca2+: 423-425nm (associated with deep blue-violet fluorescence)
Sm2+ repl. Ca2+: 708, 733nm
Yb2+ repl. Ca2+: 550nm
Dy3+:468, 478, 575, 654, 658, 663, 671, 685nm
Tb3+:482, 484, 486, 492, 539, 543, 544, 546, 583, 588nm
Er3+:519, 522, 528, 551, 554nm
Sm3+:561nm
Eu3+: 574, 595, 618, 622, 700nm
Nd3+: 920nm
M-center(2F+Na+): large pic at 720-745 nm
MA center charge stabilized by O2−–F  : 690 nm 
MA center charge stabilized by Na+–Ca2+ : 750nm


Spectrum: Michael Gaft, Petah Tikva, Israel. Plot: Institute of Mineralogy, University of Vienna, Austria, with permission of the authors.

Spectrum Galery:

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Comments on spectrum and activators:

Violet fluo associated with Eu2+ (420-423 nm) with peaks at 320 and 340nm (Ce3+),  decay time of Eu2+ is 600–800 ns
yellow fluo associated with Dy3+;
M-center: large pic at 720 nm;
Lifetime: 2μs ( @420nm);

λex = 415 nm is most suitable for measuring the Ho3+ emission beside the Er3+

Fluorite was one of the first mineral substances being investigated by George G. Stokes in 1852, hence the name fluorescence given at the phenomenon.

Fluorite is a reservoir for many of the rare earth elements. As early as 1881, it was pointed out that Cerium was present in fluorite.

In 1906, Urbain studied the cathodoluminescence of fluorite and ascribed the cause of fluorescence to RRE (Yttrium, praeseodymium, samarium, dysprosium, europium, terbium and also gadolinium and Ytterbium in chlorophane); Morse (1907), Tanaka (1924), Nichols (1928) and F. G. Wick also investigated the cause of luminescence of fluorite. 

The fusion of fluorescent fluorite (1100-1200°C) changes the spectrum markedly. Often the blue luminescence spectrum is changed to a more orange-red, showing sharp lines typical of RRE.

De Ment makes 2 groups in the luminescent fluorites:

group 1: single band in the UV at 300nm and 3 bands in the visible at 475, 508 and 578nm
group 2: two bands in UV at 280 and 300nm and strong peaks at 475, 510, 536, 548 and 578nm in the visible.

Radiation induced MA centers’ charge stabilized by Na+–Ca2+ is responsible of emission at 750nm and O2−–F at 690 nm) (Tarashchan 1978, Gaft and Al. 2020).

Best localities for fluorescence (*):

(*)The data are not exhaustive and are limited to a few remarkable localities for fluorescence

Bibliographic reference for luminescence:

Reference for luminescence on the Internet:

 

Images:

 

 

Videos:

 

Mineralogical reference on the Internet:

  http://www.mindat.org/show.php?name=Fluorite

  http://webmineral.com/data/Fluorite.shtml

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