2004
DOI: 10.1016/j.jas.2004.03.008
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Identification of black pigments on prehistoric Southwest American potsherds by infrared and Raman microscopy

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Cited by 78 publications
(62 citation statements)
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“…The band at 1320 cm -1 has been shown to broaden and shift to higher wavenumbers as the material becomes less crystalline, and in highly disordered carbon the band at 1600 cm -1 can disappear completely. The very broad nature of the bands recorded on this sample indicates the presence of amorphous carbon [17]. The lack of the phosphate Raman band at 961 cm -1 [18] and of a phosphorus peak in the EDS spectra, indicates that the carbon used is derived originally from charred plant material instead of charred bone.…”
Section: Palacio Phase (900-1200 Ad)mentioning
confidence: 84%
“…The band at 1320 cm -1 has been shown to broaden and shift to higher wavenumbers as the material becomes less crystalline, and in highly disordered carbon the band at 1600 cm -1 can disappear completely. The very broad nature of the bands recorded on this sample indicates the presence of amorphous carbon [17]. The lack of the phosphate Raman band at 961 cm -1 [18] and of a phosphorus peak in the EDS spectra, indicates that the carbon used is derived originally from charred plant material instead of charred bone.…”
Section: Palacio Phase (900-1200 Ad)mentioning
confidence: 84%
“…More recently, the use of other spectroscopic techniques has been developed, among others micro-Raman spectroscopy [8,[17][18][19][20][21], X-ray photoelectron spectroscopy (XPS) and Fourier-transform infrared spectroscopy (FTIR) [15][16][17]21], X-ray absorption (XAS and XANES) [5,22], particle-induced X-ray emission (PIXE) [23] and laserinduced breakdown spectroscopy (LIBS) [24]. On the methodological side the interest in applying such spectroscopic techniques is mainly related to the possibility of a non-destructive and/or compound-specific analysis.…”
Section: Introductionmentioning
confidence: 99%
“…3b [33]. In a red/brown spot in the translucent blue sample, typical bands of an iron oxide structure (haematite, aFe 2 O 3 ) appear at 220, 289, 398 and 1317 cm -1 [34,35] as shown in Fig. 3c.…”
Section: Blue Tesseraementioning
confidence: 82%