“…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.…”