“…Among the pioneering research, Wainwright in 1927 proposed the determination of refraction index and density of obsidian artefacts for their archaeometric characterization; successively other techniques were used, for provenance determination of obsidian artefacts, like optical emission spectroscopy (Cann & Renfrew, 1964); instrumental neutron activation analysis (Gordus, Wright, & Griffin, 1968); fission track dating (Bigazzi, Bonadonna, Belluomini, & Malpieri, 1971); energy and wavelength dispersive X-ray fluorescence using peak intensity ratios of various elements (Nelson, D'Auria, & Bennett, 1975;De Francesco, Crisci, & Bocci, 2008, respectively); particle induced X-ray emission (Nielson, Hill, Mangelson, & Nelson, 1976); electron microprobe (Merrik & Brown, 1984 ); inductively-coupled plasma mass spectrometry (ICP-MS), with or without laser ablation (Tykot &Young, 1996 andGratuze, 1999, respectively); gamma rays (Shackley, 1998); scanning electron microscopy coupled with energy dispersive spectrometer (Acquafredda, Andriani, Lorenzoni, & Zanettin, 1999); electron spin resonance (Duttine, Villeneuve, Poupeau, Rossi, & Scorzelli, 2003); Mössbauer spectroscopy (Stewart et al, 2003); Raman micro-spectroscopy (Bellot-Gurlet, Le Bourdonnec, Popeau, & Dubernet, 2004); portable or handheld portable energy dispersive spectrometers (Phillips & Speakman, 2009;Frahm, Doonan, & Kilikoglou, 2014 respectively) and recently laser-induced breakdown spectroscopy (Syvilay, Bousquet, Chapoulie, Orange, & Le Bourdonnec, 2019).…”