2015
DOI: 10.1016/j.jasrep.2014.11.007
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Reassessing obsidian field relationships at Glass Buttes, Oregon

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Cited by 8 publications
(9 citation statements)
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“…Our pXRF data also confirm these obsidian source identifications (Figure 11). These four trace elements --Nb, Sr, Rb, and Zr -are very well measured using pXRF, exhibiting the greatest repeatability and reproducibility (e.g., Grave et al, 2011;Frahm and Feinberg, 2015). The EMPA and pXRF values used to produce these scatterplots are available in Table 2 and Supplementary Table D, respectively.…”
Section: -New Domuztepe Sourcing Resultsmentioning
confidence: 99%
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“…Our pXRF data also confirm these obsidian source identifications (Figure 11). These four trace elements --Nb, Sr, Rb, and Zr -are very well measured using pXRF, exhibiting the greatest repeatability and reproducibility (e.g., Grave et al, 2011;Frahm and Feinberg, 2015). The EMPA and pXRF values used to produce these scatterplots are available in Table 2 and Supplementary Table D, respectively.…”
Section: -New Domuztepe Sourcing Resultsmentioning
confidence: 99%
“…A subset of the artifacts (43 of 66; i.e., those still available for analysis) were subsequently analyzed by portable X-ray fluorescence (pXRF), specifically a Thermo Scientific Niton XL3t GOLDD instrument at the University of Minnesota, as an independent means to corroborate our obsidian source identifications. The use of pXRF in obsidian artifact sourcing is now well attested worldwide (see Frahm, 2014b;Frahm and Feinberg, 2015; and the references within). The instrument that we used has a miniaturized 50-kV, Ag-anode X-ray tube.…”
Section: -Methods and Materialsmentioning
confidence: 99%
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“…These data were further corrected using fundamental parameters (FP), which adjusts measurements for other phenomena that occur within a specimen (e.g., X-ray absorption, secondary fluorescence). Our calibration is based on a suite of 24 obsidian custom standards characterized by neutron activation analysis (NAA) and laboratory-based XRF at the University of Missouri's Research Reactor and by electron microprobe analysis (EMPA) at the University of Minnesota (see Frahm, 2014, Frahm et al, 2014b, and Frahm and Feinberg, 2015. This approach has been shown to yield high accuracy and sensitivity (Frahm, 2014;Frahm et al, 2014b;Frahm and Feinberg, 2015).…”
Section: Geochemical Sourcing Of Lkt1 Artifactsmentioning
confidence: 99%
“…Our calibration is based on a suite of 24 obsidian custom standards characterized by neutron activation analysis (NAA) and laboratory-based XRF at the University of Missouri's Research Reactor and by electron microprobe analysis (EMPA) at the University of Minnesota (see Frahm, 2014, Frahm et al, 2014b, and Frahm and Feinberg, 2015. This approach has been shown to yield high accuracy and sensitivity (Frahm, 2014;Frahm et al, 2014b;Frahm and Feinberg, 2015). Routine measurements of larger artifacts often take 10-40 seconds using our methods; however, for this study, each measurement took 60 seconds in order to attain suitable counting statistics using the small-spot collimator.…”
Section: Geochemical Sourcing Of Lkt1 Artifactsmentioning
confidence: 99%