Lijst van fluorescerende mineralen


Scheikundige formule: (Na,Ca)3(Sr,Ba,Ce)3(CO3)5

Familie: Carbonaten

Status: IMA-GP

Kristal Systeem: Hexagonal

Mineraal om tentoon te stellen: Nee


UV Type Kleur Intensiteit Frequentie van de observatie
Lange Golven (365nm):      Oranje rood (Zalmkleurig)
Midden Golven (320 nm):      Blauw wit
Korte Golven(254 nm):      Oranje rood (Zalmkleurig)
Andere kleuren lange golven:     
Roze ,
Andere kleuren korte golven:          
Blauw wit , Roze ,

Fosforescentie (in de algemene betekenis) zien met het blote oog:

No Data


Specimen not analyzed. should be strictly speaking labeled burbankite group (in the sense of Horvath – Lapis, Rivista 2000). Other possibilities for not analysed specimens: remondite(Ce), petersenite-(Ce), khanneshite and calcioburbankite. 

Activator en spectrum:

Voornaamste Activator: Fe3+

Andere activatoren: Ce3+ , Sm3+ , Eu3+ , Dy3+ , Mn2+ , O* , Nd3+ ,

Pieks in het spectrum (nm):

Ce3+ repl. Ca2+ : 390nm 

Mn2+ repl. Ca2+ : 560nm 

Sm3+ : 560 - 561, 594, 600, 642, 650, 702nm  (exc.532nm)

Eu3+ : 616nm

Fe3+  : 735nm 

Nd3+ repl. Ca2+ :869, 898, 950nm (exc. 780nm)

Geen spectrum voor de moment

Commentaar over activators en spectra:

Laser-induced photoluminescence was studied for burbankite group minerals hexagonal burbankite, calcioburbankite, khanneshite and monoclinic remondite-(Ce), remondite-(La), petersenite-(Ce), as well as for orthorhombic carbocemaite and strontianite from carbonatites and hydrothennalites of alkaline complexes from various regions of the world.


Burbankite was studied by steady-state luminescence spectroscopy and luminescence of trivalent REE, such as Dy, Sm and Nd, was found (Gorobets and Rogojine 2001)


All REE-rich minerals of burbankite group (REЕ2Оз ~ 10.5 wt%) are characterized by violet luminescence and their photo- and X-ray luminescence spectra always contail1 four bands of Sm3+.

Low-REE hydrothermal burbankites (RЕЕ2Оз < 3 wt%) are distinguished bу different luminescence colors (from whitish to violet) and the low intensive spectra without Sm3+ bands.

The essential differences in luminescence properties of indicated burbankites are determined bу concentration ratio of the luminogene donor (Се3+) and the luminogene acceptor (Sm3+). (Gaft)


Beste vindplaats voor fluorescentie(*):

(*)Gegevens zijn niet exhaustieve, ze zijn beperkt tot de meest belangrijke plaatsen voor fluorescentie

Referentie voor fluorescentie:

Referentie voor luminenscentie op het internet:

Mineralogische Referentie op het internet:

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  Onderzoek op Wikipédia


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Snel opzoeking van een fluorescerend mineraal: