Please use this identifier to cite or link to this item: https://ir.swu.ac.th/jspui/handle/123456789/13574
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dc.contributor.authorHuong L.T.-T.
dc.contributor.authorVuong B.S.
dc.contributor.authorThuyet N.T.M.
dc.contributor.authorKhoi N.N.
dc.contributor.authorSatitkune S.
dc.contributor.authorWanthanachaisaeng B.
dc.contributor.authorHofmeister W.
dc.contributor.authorHäger T.
dc.contributor.authorHauzenberger C.
dc.date.accessioned2021-04-05T03:24:45Z-
dc.date.available2021-04-05T03:24:45Z-
dc.date.issued2016
dc.identifier.issn13554565
dc.identifier.other2-s2.0-85010639094
dc.identifier.urihttps://ir.swu.ac.th/jspui/handle/123456789/13574-
dc.identifier.urihttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85010639094&doi=10.15506%2fJoG.2016.35.4.308&partnerID=40&md5=47b894259768f88ad69f661b9965a725
dc.description.abstractGem-quality brown zircon occurs in alluvial deposits derived from Neogene- Quaternary alkali basalts in the Central Highlands of Vietnam. Rough and cut samples were characterized using standard gemmological methods, chemical analysis (electron microprobe and LA-ICP-MS), and Raman, FTIR and UVVis- NIR spectroscopy. Among the internal features observed were colour zoning and various mineral inclusions, such as apatite, ilmenite, hematite and iron hydroxide. The analysed samples contained up to 1.14 wt.% HfO2 and 0.08 wt.% total REE oxides. Darker brown stones contained greater amounts of Hf than the lighter-coloured ones. Raman and FTIR spectroscopy showed that the zircon is high-type (i.e. has high crystallinity). As with the famous Ratanakiri zircon of neighbouring Cambodia, heat treatments can be applied to dark-coloured samples to lighten the coloration in an oxidizing atmosphere or induce blue colour in reducing conditions. © 2016 The Gemmological Association of Great Britain.
dc.titleGeology, gemmological properties and preliminary heat treatment of gem-quality zircon from the central highlands of Vietnam
dc.typeArticle
dc.rights.holderScopus
dc.identifier.bibliograpycitationJournal of Gemmology. Vol 35, No.4 (2016), p.308-318
dc.identifier.doi10.15506/JoG.2016.35.4.308
Appears in Collections:Scopus 1983-2021

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