TY - JOUR
T1 - Luminescent centres in pezzottaite, CsBe2LiAl2Si 6O18
AU - Panczer, Gérard
AU - Gaft, Michael
AU - De Ligny, Dominique
AU - Boudeulle, Micheline
AU - Champagnon, Bernard
PY - 2010
Y1 - 2010
N2 - Pezzottaite, CsBe2LiAl2Si6O18, is a rare new pink mineral found in central Madagascar and Afghanistan, exhibiting a beryl-like trigonal reduced symmetry (R3c). Numerous data on its optical properties, Raman, IR, absorption spectra as well LIBS data are available, while it is described as a non-luminescent mineral under UV light. However, pezzottaite shows several laser-induced red emissions and a particular unusual blue luminescence. LIBS analysis reveals the presence of Sc, Ca, Sr, Na, K and Rb as substituted trace elements, but these elements cannot be considered as the centres responsible for the observed emissions. Timeresolved analyses under different excitations (266, 355, 514 and 532 nm) at room and liquid nitrogen temperatures allow the identification of Fe3+ (730 nm) and Cr3+ (699 nm) as red emitting centres, while Tl+ is considered responsible for the blue fluorescence (420-425 nm). Photoluminescence proves effective for identifying the presence of these luminescent trace elements even below the LIBS detection limit (a few ppm), but without yet attaining a quantitative resolution.
AB - Pezzottaite, CsBe2LiAl2Si6O18, is a rare new pink mineral found in central Madagascar and Afghanistan, exhibiting a beryl-like trigonal reduced symmetry (R3c). Numerous data on its optical properties, Raman, IR, absorption spectra as well LIBS data are available, while it is described as a non-luminescent mineral under UV light. However, pezzottaite shows several laser-induced red emissions and a particular unusual blue luminescence. LIBS analysis reveals the presence of Sc, Ca, Sr, Na, K and Rb as substituted trace elements, but these elements cannot be considered as the centres responsible for the observed emissions. Timeresolved analyses under different excitations (266, 355, 514 and 532 nm) at room and liquid nitrogen temperatures allow the identification of Fe3+ (730 nm) and Cr3+ (699 nm) as red emitting centres, while Tl+ is considered responsible for the blue fluorescence (420-425 nm). Photoluminescence proves effective for identifying the presence of these luminescent trace elements even below the LIBS detection limit (a few ppm), but without yet attaining a quantitative resolution.
KW - LIBS
KW - Luminescence
KW - Pezzottaite
KW - Trace elements
UR - http://www.scopus.com/inward/record.url?scp=77957713364&partnerID=8YFLogxK
U2 - 10.1127/0935-1221/2010/0022-2039
DO - 10.1127/0935-1221/2010/0022-2039
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AN - SCOPUS:77957713364
SN - 0935-1221
VL - 22
SP - 605
EP - 612
JO - European Journal of Mineralogy
JF - European Journal of Mineralogy
IS - 4
ER -