Archaeologia Islandica - 01.01.2009, Qupperneq 49

Archaeologia Islandica - 01.01.2009, Qupperneq 49
Geochemical Identification of Obsidian Artifacts Trace Elements Cat. No. Rb Sr Y Zr Nb Ba Chemical Tvne NI-3532 80 130 94 895 116 662 Katla (This analysis) ±4 ±3 ±4 ±4 ±3 ±18 NI-3532 (Jónasson 2007)a, 78 128 96 1004 114 726 Katla NI-21680 64 63 162 362 82 459 Hágöngur (This analysis) ±4 ±3 ±4 ±4 ±3 ±18 NI-21680 (Jónasson, unpublished data) 64 67 183 404 97 518 Hágöngur NI-21702 123 15 118 1135 164 161 Torfajökull (This analysis) ±4 ±3 ±4 ±4 ±3 ±18 NI-21702 (Jónasson 2007)a 123 14 133 1270 166 187 Torfajökull NI-21839 86 64 117 477 135 787 Kerlingarfjöll (This analysis) ±4 ±3 ±4 ±4 ±3 ±18 NI-21839 (Jónasson 2007)a 83 64 121 537 143 855 Kerlingarfjöll NI-24189b 62 97 99 497 56 537 Krafla (This analysis) ±4 ±3 ±3 ±4 ±3 ±14 NI-21969 (Jónasson 2007) 77 91 111 441 52 590 Krafla Sample # 14 (Jónasson 1994: Table 3) 66 97 98 475 52 524 Krafla Note: a, Comparative data from Jónasson (1994: Table 3; 2007: Tablel) rounded to the nearest ppm. b, At the time of this writing Jónasson had no measurements on Krafla sample NI-24189, but he wrote to the senior author that data published for sample NI-21969 from Krafla should represent the same composition as NI-24189 (Jónasson, personal communication). Katla chemical type sampled from Kriki; Kerlingarfjöll sampled from Ogmundur; Torfajökull sampled at Hrafntinnusker; Krafla samples represent the third phase of rhyolite volcanism; NI-21969 sampled from Hlíðarfjall. Table 3. Comparison of Trace Element Concentration Measurements for Five Icelandic Obsidians Laboratory Analysis Non-destructive energy dispersive x-ray fluorescence (edxrf) analysis of the four Hofstaðir obsidian artifacts was con- ducted by the senior author using a QuanX-EC™ (Thermo Electron Corporation) edxrf spectrometerequipped with a silver (Ag) x-ray tube, a 50 kV x-ray generator, digital pulse processor with automated energy calibration, and a Peltier cooled solid state detector with 145 eV resolution (FWHM) at 5.9 keV. The x-ray tube was operated at differing voltage and current settings to optimize 47
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Archaeologia Islandica

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