TY - JOUR
T1 - Green-luminescing hyalite opal from zacatecas, Mexico
AU - Fritsch, Emmanuel
AU - Megaw, Peter K.M.
AU - Spano, Tyler L.
AU - Chauviré, Boris
AU - Rondeau, Benjamin
AU - Gray, Michael
AU - Hainschwang, Thomas
AU - Renfro, Nathan
N1 - Publisher Copyright:
© 2015 The Gemmological Association of Great Britain.
PY - 2015
Y1 - 2015
N2 - Green daylight-fluorescing hyalite opal was discovered in Mexico's Zacatecas State in 2013. It occurs as botryoidal coatings commonly up to 1 cm thick along fractures and cavities in a poorly welded rhyolitic tuff. The material possesses spectacular colour behaviour, appearing near-colourless or pale-tomoderate yellow in incandescent light and vivid greenish yellow to yellowish green in indirect sunlight. The daylight-induced green luminescence is related to the presence of trace amounts of the uranyl molecule (UO2)2+. Several dozen high-quality transparent gemstones in the 1-6+ ct range have been faceted from this material so far, in addition to hundreds of smaller stones. The gems typically contain two-phase fluid inclusions and curved deposition marks, and they show bright interference colour patterns between crossed polarizers. This hyalite is not porous, and contains approximately 2.7 wt.% H2O, which is remarkably low among gem opals. The radioactivity of the opal is within background levels, and does not pose any health concern.
AB - Green daylight-fluorescing hyalite opal was discovered in Mexico's Zacatecas State in 2013. It occurs as botryoidal coatings commonly up to 1 cm thick along fractures and cavities in a poorly welded rhyolitic tuff. The material possesses spectacular colour behaviour, appearing near-colourless or pale-tomoderate yellow in incandescent light and vivid greenish yellow to yellowish green in indirect sunlight. The daylight-induced green luminescence is related to the presence of trace amounts of the uranyl molecule (UO2)2+. Several dozen high-quality transparent gemstones in the 1-6+ ct range have been faceted from this material so far, in addition to hundreds of smaller stones. The gems typically contain two-phase fluid inclusions and curved deposition marks, and they show bright interference colour patterns between crossed polarizers. This hyalite is not porous, and contains approximately 2.7 wt.% H2O, which is remarkably low among gem opals. The radioactivity of the opal is within background levels, and does not pose any health concern.
UR - http://www.scopus.com/inward/record.url?scp=84975763854&partnerID=8YFLogxK
U2 - 10.15506/JoG.2015.34.6.490
DO - 10.15506/JoG.2015.34.6.490
M3 - Article
AN - SCOPUS:84975763854
SN - 1355-4565
VL - 34
SP - 490
EP - 508
JO - Journal of Gemmology
JF - Journal of Gemmology
IS - 6
ER -