SPHALERITE

 


Chemical formula: (Zn,Fe)S

Family: Sulfide

Status: IMA-GP

Crystal system : Isometric

Display mineral: OUI

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

 

Luminescence:

Longwave UV (365nm) colors:

                             


Orange , Pale Yellow , Yellow , Orangy yellow , Greenish Yellow , Yellowish ,

Intensity LW:Strong

Midwave UV (320nm) colors:

                             


Orange , Pale Yellow , Yellow , Orangy yellow , Greenish Yellow , Yellowish ,

Intensity MW:Strong

Shortwave UV (254nm) colors:

                             


Orange , Pale Yellow , Yellow , Orangy yellow , Greenish Yellow , Yellowish ,

Intensity SW:Medium


Daylight picture


SPHALERITE;
Franklin Mine, Franklin Mining District, Sussex Co., New Jersey, USA
Photo and Copyright:
Middleearthminerals.com
Used with permission of the author

Longwave (365nm) picture


SPHALERITE;
Franklin Mine, Franklin Mining District, Sussex Co., New Jersey, USA
UVLW, Photo and Copyright:
Middleearthminerals.com
Used with permission of the author

Shortwave (254nm) picture


SPHALERITE;
Franklin Mine, Franklin Mining District, Sussex Co., New Jersey, USA
UVSW, Photo and Copyright:
Middleearthminerals.com
Used with permission of the author

 

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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):

Pale Yellow

UV moyens (320 nm):

Pale Yellow

UV courts (254 nm):

Pale Yellow
 

Triboluminescence: OUI

Thermoluminescence: OUI

Comments:

synonyme: blende ; brunckite = colloïdal sphalerite  ;

variety cleiophane: orange SW and LW;

Activator(s) and spectrum:

Activator(s): Mn2+ , Cu+,  

Peaks in the spectrum (nm):

Mn2+ replacing Zn2+ : large band peaking at 595 nm 

VZn-Cl- : 450-460-470nm

Cu+-Ga3+, Cu+-In3+ repl Zn2+ : 640-670-675nm 

No spectrum yet

Comments on spectrum and activators:

Ed. Becqurel studied the decay of the phosphorescence of the different component (bands) of the spectrum of ZnS, proposing a number of mathemetical expression to interpret this phenomenon (1860).

One of the oldest studies on activator in zinc sulphide was made by H. Grune (1904). He noted that a small amont of manganese in ZnS produced an orange luminescence and triboluminescence in a very similar way as the natural mineral. Jorrissen and Ringe (1904) also studied zinc sulfide fluorescence.

The influence of the irradiation by a red light and infrared radiations upon the photoluminescence has been studied by C. Peirce (1906) under a variety of conditions.

Nichols found the presence of 48 bands/peaks in the spectrum coinciding in part with thallium, Erbium, Ytterbium. 

[after De Ment, 1949]

 

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=Sphalerite

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

Internet Search:

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Note: While all due attention has been paid to the implementation of the database, it may contain errors and/or accidental omissions. By nature, the database will always be incomplete because science always evolves according to new analysis.
A request providing no result means only that no such reference exists in the database, but it does not mean that what you are looking for does not exist, just not to our knowledge. If you think you have found an error or omission, please let us know via the contact page being sure to cite the source of information.