2014
DOI: 10.1002/jrs.4524
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Characterization of emeralds by micro‐Raman spectroscopy

Abstract: In recent years, the use of Raman spectroscopy as a gemological tool has largely increased, in particular in the conservation science field where a non-destructive and contactless identification is required. In this work, we show the large amount of information which is possible to obtain with Raman analysis on one of the most important gems, emerald, the green variety of beryl. In particular, 14 not certified faceted emeralds have been studied by means of a standard micro-Raman spectrometer, allowing also the… Show more

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Cited by 38 publications
(51 citation statements)
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“…The most common field of application of Raman spectroscopy is the identification of mineral phases and components of geological samples on the basis of spectral fingerprint-characteristics. Examples include the fields of gemmology (e.g., Fritsch et al, 2004;Jasinevicius, 2009;Bersani and Lottici, 2010;Bersani et al, 2014), archaeometry and cultural heritage (e.g., Edwards et al, 2000;Smith, 2006;Vandenabeele et al, 2007;Ropret et al, 2010), high-pressure petrology (e.g., Korsakov et al, 2005;Stähle et al, 2008;Marschall et al, 2009), planetary mineralogy (e.g., Wang et al, 1995;Sharma et al, 2003;Wang et al, 2004;Popp and Schmitt, 2004;Bozlee et al, 2005;Blacksberg et al, 2010), environmental mineralogy (e.g., Das and Hendry, 2011), palaeontology (e.g., Schopf et al, 2002;Bernard et al, 2007;Chen et al, 2007), biomineralogy (e.g., Li et al, 2013;Pasteris et al, 2014), and many other disciplines. Furthermore, Earth scientists have become increasingly interested in the application of the hyperspectral Raman-mapping technique.…”
Section: Introductionmentioning
confidence: 98%
“…The most common field of application of Raman spectroscopy is the identification of mineral phases and components of geological samples on the basis of spectral fingerprint-characteristics. Examples include the fields of gemmology (e.g., Fritsch et al, 2004;Jasinevicius, 2009;Bersani and Lottici, 2010;Bersani et al, 2014), archaeometry and cultural heritage (e.g., Edwards et al, 2000;Smith, 2006;Vandenabeele et al, 2007;Ropret et al, 2010), high-pressure petrology (e.g., Korsakov et al, 2005;Stähle et al, 2008;Marschall et al, 2009), planetary mineralogy (e.g., Wang et al, 1995;Sharma et al, 2003;Wang et al, 2004;Popp and Schmitt, 2004;Bozlee et al, 2005;Blacksberg et al, 2010), environmental mineralogy (e.g., Das and Hendry, 2011), palaeontology (e.g., Schopf et al, 2002;Bernard et al, 2007;Chen et al, 2007), biomineralogy (e.g., Li et al, 2013;Pasteris et al, 2014), and many other disciplines. Furthermore, Earth scientists have become increasingly interested in the application of the hyperspectral Raman-mapping technique.…”
Section: Introductionmentioning
confidence: 98%
“…Emerald grew in contact with schist rocks usually contain more alkali ions than those coming from classical granitic pegmatite. Therefore, for 'non-schist type' emeralds, the intensity of 3608 cm -1 bands should be higher than that of the band at 3598 cm -1 [4].…”
Section: Raman Study Of the Inclusionsmentioning
confidence: 94%
“…[22,23,157] to precious stones selected for their aesthetic value (Lapis Lazuli, jade, nephrite, etc.) [56,72,82,155], fossilised resins (amber, copal, etc.)…”
Section: Minerals and Gemstonesmentioning
confidence: 99%