IntChron > doi > 10.1002 > jqs.1498
| labcode | batch | instrument | SiO2 | TiO2 | Al2O3 | FeOt | MnO | MgO | CaO | Na2O | K2O | P2O5 | Cl | F | total | ok | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 180507/AF555-556/1 | Tephra_56 | OXF-BEG/RLAHA-WDS | 69.87 | 0.26 | 13.39 | 3.46 | 0.13 | 0.18 | 1.17 | 4.06 | 3.33 | 0 | 0 | 0 | 95.86 | 1 | ||
| 180507/AF555-556/2 | Tephra_56 | OXF-BEG/RLAHA-WDS | 72.05 | 0 | 20.89 | 0.02 | 0 | 0.01 | 0.34 | 11.61 | 0.19 | 0 | 0 | 0 | 105.11 | 0 | ||
| 180507/AF555-556/3 | Tephra_56 | OXF-BEG/RLAHA-WDS | 71.32 | 0.27 | 13.47 | 3.59 | 0.15 | 0.2 | 1.22 | 4.61 | 3.58 | 0 | 0 | 0 | 98.41 | 1 | ||
| 180507/AF555-556/4 | Tephra_56 | OXF-BEG/RLAHA-WDS | 74.73 | 0.13 | 12.72 | 1.38 | 0.05 | 0.09 | 0.7 | 3.34 | 3.7 | 0 | 0 | 0 | 96.83 | 0 | ||
| 180507/AF555-556/5 | Tephra_56 | OXF-BEG/RLAHA-WDS | 72.75 | 0.28 | 13.86 | 3.54 | 0.12 | 0.19 | 1.19 | 4.87 | 3.66 | 0 | 0 | 0 | 100.45 | 1 | ||
| 180507/AF555-556/6 | Tephra_56 | OXF-BEG/RLAHA-WDS | 67.4 | 0.27 | 12.88 | 3.56 | 0.14 | 0.19 | 1.17 | 4.13 | 3.46 | 0 | 0 | 0 | 93.2 | 0 | ||
| 180507/AF555-556/7 | Tephra_56 | OXF-BEG/RLAHA-WDS | 66.91 | 0.03 | 19.15 | 0 | 0 | 0 | 0.01 | 0.73 | 15.51 | 0 | 0 | 0 | 102.34 | 0 | ||
| 180507/AF555-556/8 | Tephra_56 | OXF-BEG/RLAHA-WDS | 72.69 | 0.25 | 13.76 | 3.58 | 0.14 | 0.21 | 1.22 | 4.25 | 3.7 | 0 | 0 | 0 | 99.81 | 1 | ||
| 180507/AF555-556/9 | Tephra_56 | OXF-BEG/RLAHA-WDS | 72.12 | 0.24 | 13.79 | 3.54 | 0.15 | 0.19 | 1.18 | 4.12 | 3.54 | 0 | 0 | 0 | 98.87 | 1 | ||
| 180507/AF555-556/10 | Tephra_56 | OXF-BEG/RLAHA-WDS | 69.03 | 0.23 | 13.13 | 3.43 | 0.15 | 0.2 | 1.15 | 4.25 | 3.32 | 0 | 0 | 0 | 94.89 | 1 | ||
| ipm2011ecc_ed/AF555/08 | matthews2011ecc2 | EDIN-TAU-WDS | 74.343 | 0.118 | 12.508 | 1.363 | 0.043 | 0.079 | 0.693 | 3.913 | 3.807 | 0.009 | 0.119 | 0.096 | 97.091 | 0 | ||
| ipm2011ecc_ed/AF555/09 | matthews2011ecc2 | EDIN-TAU-WDS | 73.5 | 0.279 | 13.442 | 3.946 | 0.165 | 0.181 | 1.244 | 5.137 | 3.448 | 0.033 | 0.166 | 0.179 | 101.745 | 1 | ||
| ipm2011ecc_ed/AF555/10 | matthews2011ecc2 | EDIN-TAU-WDS | 72.786 | 0.278 | 13.059 | 3.708 | 0.149 | 0.188 | 1.269 | 5.082 | 3.565 | 0.02 | 0.169 | 0.218 | 100.502 | 1 | ||
| ipm2011ecc_ed/AF555/11 | matthews2011ecc2 | EDIN-TAU-WDS | 72.383 | 0.274 | 13.185 | 3.698 | 0.149 | 0.207 | 1.278 | 4.903 | 3.529 | 0.036 | 0.162 | 0.196 | 100.011 | 1 | ||
| ipm2011ecc_ed/AF555/12 | matthews2011ecc2 | EDIN-TAU-WDS | 71.935 | 0.273 | 13.177 | 3.876 | 0.144 | 0.17 | 1.237 | 4.778 | 3.675 | 0.041 | 0.146 | 0.212 | 99.674 | 1 |
| labcode | batch | instrument | SiO2 | TiO2 | Al2O3 | FeOt | MnO | MgO | CaO | Na2O | K2O | P2O5 | Cl | F | total | ok | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 180507/AF638-639/1 | Tephra_56 | OXF-BEG/RLAHA-WDS | 73.08 | 0.12 | 12.41 | 1.49 | 0.06 | 0.09 | 0.72 | 3.49 | 3.71 | 0 | 0 | 0 | 95.18 | 1 | ||
| 180507/AF638-639/2 | Tephra_56 | OXF-BEG/RLAHA-WDS | 71.05 | 0.13 | 12.08 | 1.38 | 0.02 | 0.08 | 0.7 | 3.45 | 3.69 | 0 | 0 | 0 | 92.56 | 0 | ||
| 180507/AF638-639/3 | Tephra_56 | OXF-BEG/RLAHA-WDS | 71.79 | 0.11 | 12.15 | 1.32 | 0.01 | 0.08 | 0.71 | 2.99 | 3.73 | 0 | 0 | 0 | 92.89 | 0 | ||
| 180507/AF638-639/4 | Tephra_56 | OXF-BEG/RLAHA-WDS | 67.64 | 0.1 | 11.55 | 1.36 | 0.08 | 0.06 | 0.68 | 2.79 | 3.54 | 0 | 0 | 0 | 87.79 | 0 | ||
| 180507/AF638-639/5 | Tephra_56 | OXF-BEG/RLAHA-WDS | 69.26 | 0.13 | 11.97 | 1.34 | 0.03 | 0.07 | 0.68 | 3.13 | 3.6 | 0 | 0 | 0 | 90.21 | 0 | ||
| 180507/AF638-639/6 | Tephra_56 | OXF-BEG/RLAHA-WDS | 66.22 | 0 | 20.26 | 0.24 | 0 | 0.03 | 0.56 | 10.28 | 0.51 | 0 | 0 | 0 | 98.1 | 0 | ||
| 180507/AF638-639/7 | Tephra_56 | OXF-BEG/RLAHA-WDS | 61.29 | 0 | 24.71 | 0.03 | 0 | 0 | 6.18 | 7.75 | 0.22 | 0 | 0 | 0 | 100.17 | 0 | ||
| 180507/AF638-639/8 | Tephra_56 | OXF-BEG/RLAHA-WDS | 64.36 | 0 | 21.15 | 0.02 | 0.01 | 0 | 2.53 | 9.77 | 0.1 | 0 | 0 | 0 | 97.95 | 0 | ||
| 180507/AF638-639/9 | Tephra_56 | OXF-BEG/RLAHA-WDS | 72.43 | 0.14 | 12.27 | 1.45 | 0.05 | 0.09 | 0.75 | 3.3 | 3.83 | 0 | 0 | 0 | 94.31 | 1 | ||
| 180507/AF638-639/10 | Tephra_56 | OXF-BEG/RLAHA-WDS | 71.83 | 0.12 | 12.2 | 1.46 | 0.04 | 0.08 | 0.72 | 3.28 | 3.73 | 0 | 0 | 0 | 93.45 | 0 | ||
| 180507/AF638-639/11 | Tephra_56 | OXF-BEG/RLAHA-WDS | 72.52 | 0.12 | 12.33 | 1.42 | 0.05 | 0.08 | 0.71 | 3.3 | 3.75 | 0 | 0 | 0 | 94.28 | 1 | ||
| 180507/AF638-639/12 | Tephra_56 | OXF-BEG/RLAHA-WDS | 72.66 | 0.13 | 12.3 | 1.48 | 0.06 | 0.1 | 0.73 | 3.44 | 3.84 | 0 | 0 | 0 | 94.72 | 1 | ||
| 180507/AF638-639/13 | Tephra_56 | OXF-BEG/RLAHA-WDS | 72.86 | 0.13 | 12.34 | 1.46 | 0.04 | 0.07 | 0.76 | 3.3 | 3.78 | 0 | 0 | 0 | 94.73 | 1 | ||
| 180507/AF638-639/14 | Tephra_56 | OXF-BEG/RLAHA-WDS | 64.55 | 0 | 18.47 | 0 | 0 | 0 | 0 | 0.74 | 15.84 | 0 | 0 | 0 | 99.59 | 0 | ||
| 180507/AF638-639/15 | Tephra_56 | OXF-BEG/RLAHA-WDS | 72.54 | 0.14 | 12.23 | 1.45 | 0.03 | 0.07 | 0.69 | 3.39 | 3.78 | 0 | 0 | 0 | 94.32 | 1 | ||
| 180507/AF638-639/16 | Tephra_56 | OXF-BEG/RLAHA-WDS | 71.49 | 0.11 | 12.02 | 1.41 | 0.05 | 0.09 | 0.69 | 3.34 | 3.72 | 0 | 0 | 0 | 92.9 | 0 | ||
| 180507/AF638-639/17 | Tephra_56 | OXF-BEG/RLAHA-WDS | 67.16 | 0.12 | 11.36 | 1.31 | 0.01 | 0.08 | 0.66 | 3.1 | 3.49 | 0 | 0 | 0 | 87.29 | 0 | ||
| 180507/AF638-639/18 | Tephra_56 | OXF-BEG/RLAHA-WDS | 73.28 | 0.11 | 12.43 | 1.4 | 0.01 | 0.09 | 0.75 | 3.22 | 3.78 | 0 | 0 | 0 | 95.05 | 1 | ||
| 180507/AF638-639/19 | Tephra_56 | OXF-BEG/RLAHA-WDS | 71.88 | 0.1 | 12.06 | 1.44 | 0 | 0.09 | 0.71 | 3.27 | 3.84 | 0 | 0 | 0 | 93.38 | 0 | ||
| 180507/AF638-639/20 | Tephra_56 | OXF-BEG/RLAHA-WDS | 64.21 | 0 | 18.46 | 0.02 | 0.02 | 0.01 | 0.01 | 0.5 | 15.73 | 0 | 0 | 0 | 98.97 | 0 |
| labcode | batch | instrument | SiO2 | TiO2 | Al2O3 | FeOt | MnO | MgO | CaO | Na2O | K2O | P2O5 | Cl | F | total | ok | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 180507/AF672-673/1 | Tephra_56 | OXF-BEG/RLAHA-WDS | 72.58 | 0.15 | 12.23 | 1.46 | 0.03 | 0.07 | 0.71 | 3.34 | 3.78 | 0 | 0 | 0 | 94.35 | 1 | ||
| 180507/AF672-673/2 | Tephra_56 | OXF-BEG/RLAHA-WDS | 73.58 | 0.14 | 12.53 | 1.44 | 0 | 0.08 | 0.77 | 3.45 | 3.68 | 0 | 0 | 0 | 95.66 | 1 | ||
| 180507/AF672-673/3 | Tephra_56 | OXF-BEG/RLAHA-WDS | 71.29 | 0.14 | 11.98 | 1.46 | 0.05 | 0.08 | 0.73 | 1.46 | 5.67 | 0 | 0 | 0 | 92.84 | 0 | ||
| 180507/AF672-673/4 | Tephra_56 | OXF-BEG/RLAHA-WDS | 73.7 | 0.13 | 12.41 | 1.39 | 0.05 | 0.08 | 0.75 | 3.66 | 3.83 | 0 | 0 | 0 | 95.98 | 1 | ||
| 180507/AF672-673/5 | Tephra_56 | OXF-BEG/RLAHA-WDS | 73.61 | 0.15 | 12.56 | 1.54 | 0.04 | 0.11 | 0.77 | 3.61 | 3.77 | 0 | 0 | 0 | 96.15 | 1 | ||
| 180507/AF672-673/6 | Tephra_56 | OXF-BEG/RLAHA-WDS | 70.72 | 0.13 | 12.22 | 1.5 | 0.03 | 0.07 | 0.72 | 3.34 | 3.57 | 0 | 0 | 0 | 92.31 | 0 | ||
| 180507/AF672-673/7 | Tephra_56 | OXF-BEG/RLAHA-WDS | 65.09 | 0.01 | 18.64 | 0 | 0 | 0 | 0 | 0.65 | 15.71 | 0 | 0 | 0 | 100.1 | 0 | ||
| 180507/AF672-673/8 | Tephra_56 | OXF-BEG/RLAHA-WDS | 72.78 | 0.14 | 12.39 | 1.49 | 0.03 | 0.09 | 0.73 | 3.4 | 3.83 | 0 | 0 | 0 | 94.88 | 1 | ||
| 180507/AF672-673/9 | Tephra_56 | OXF-BEG/RLAHA-WDS | 74.57 | 0.15 | 12.63 | 1.41 | 0.03 | 0.07 | 0.72 | 3.65 | 3.76 | 0 | 0 | 0 | 96.99 | 1 | ||
| 180507/AF672-673/10 | Tephra_56 | OXF-BEG/RLAHA-WDS | 73.69 | 0.13 | 12.36 | 1.47 | 0.06 | 0.08 | 0.73 | 3.43 | 3.85 | 0 | 0 | 0 | 95.81 | 1 | ||
| 180507/AF672-673/11 | Tephra_56 | OXF-BEG/RLAHA-WDS | 64.66 | 0.03 | 18.62 | 0.03 | 0.05 | 0 | 0.04 | 0.92 | 15.34 | 0 | 0 | 0 | 99.69 | 0 | ||
| 180507/AF672-673/12 | Tephra_56 | OXF-BEG/RLAHA-WDS | 73.7 | 0.14 | 12.51 | 1.51 | 0.06 | 0.09 | 0.77 | 3.55 | 3.79 | 0 | 0 | 0 | 96.11 | 1 | ||
| 180507/AF672-673/13 | Tephra_56 | OXF-BEG/RLAHA-WDS | 72.53 | 0.12 | 12.24 | 1.46 | 0.06 | 0.06 | 0.74 | 3.44 | 3.74 | 0 | 0 | 0 | 94.39 | 1 | ||
| 180507/AF672-673/14 | Tephra_56 | OXF-BEG/RLAHA-WDS | 66.05 | 0.01 | 18.57 | 0.04 | 0 | 0 | 0.01 | 0.64 | 15.88 | 0 | 0 | 0 | 101.2 | 0 | ||
| 180507/AF672-673/15 | Tephra_56 | OXF-BEG/RLAHA-WDS | 64.37 | 0 | 18.29 | 0.03 | 0 | 0 | 0.01 | 0.76 | 15.63 | 0 | 0 | 0 | 99.09 | 0 |
| labcode | batch | instrument | SiO2 | TiO2 | Al2O3 | FeOt | MnO | MgO | CaO | Na2O | K2O | P2O5 | Cl | F | total | ok | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| ipm2011ecc/AF591/01 | matthews2011ecc1 | OX-ES-WDS1 | 74.25 | 0.118 | 12.594 | 1.423 | 0.047 | 0.075 | 0.742 | 2.49 | 3.986 | 0 | 0 | 0 | 95.725 | 0 | ||
| ipm2011ecc/AF591/02 | matthews2011ecc1 | OX-ES-WDS1 | 73.156 | 0.152 | 12.446 | 1.427 | 0.034 | 0.073 | 0.733 | 3.139 | 3.77 | 0 | 0 | 0 | 94.93 | 0 | ||
| ipm2011ecc/AF591/03 | matthews2011ecc1 | OX-ES-WDS1 | 72.96 | 0.297 | 13.711 | 3.731 | 0.145 | 0.22 | 1.277 | 1.524 | 3.546 | 0 | 0 | 0 | 97.411 | 1 | ||
| ipm2011ecc/AF591/04 | matthews2011ecc1 | OX-ES-WDS1 | 72.685 | 0.257 | 13.672 | 3.716 | 0.12 | 0.187 | 1.196 | 2.852 | 3.79 | 0 | 0 | 0 | 98.475 | 1 | ||
| ipm2011ecc/AF591/05 | matthews2011ecc1 | OX-ES-WDS1 | 72.369 | 0.265 | 13.652 | 3.642 | 0.153 | 0.2 | 1.199 | 4.028 | 3.723 | 0 | 0 | 0 | 99.231 | 1 | ||
| ipm2011ecc/AF591/06 | matthews2011ecc1 | OX-ES-WDS1 | 72.036 | 0.279 | 13.732 | 3.624 | 0.143 | 0.226 | 1.241 | 4.083 | 3.536 | 0 | 0 | 0 | 98.9 | 1 | ||
| ipm2011ecc/AF591/07 | matthews2011ecc1 | OX-ES-WDS1 | 71.395 | 0.327 | 13.634 | 3.67 | 0.165 | 0.22 | 1.267 | 2.851 | 3.541 | 0 | 0 | 0 | 97.07 | 1 | ||
| ipm2011ecc/AF591/08 | matthews2011ecc1 | OX-ES-WDS1 | 70.839 | 0.26 | 13.44 | 3.546 | 0.142 | 0.196 | 1.293 | 3.589 | 3.514 | 0 | 0 | 0 | 96.819 | 1 | ||
| ipm2011ecc/AF591/09 | matthews2011ecc1 | OX-ES-WDS1 | 70.654 | 0.288 | 13.424 | 3.707 | 0.148 | 0.202 | 1.266 | 3.251 | 3.639 | 0 | 0 | 0 | 96.579 | 1 | ||
| ipm2011ecc/AF591/10 | matthews2011ecc1 | OX-ES-WDS1 | 69.394 | 0.257 | 13.213 | 3.426 | 0.15 | 0.22 | 1.179 | 3.531 | 3.358 | 0 | 0 | 0 | 94.728 | 1 | ||
| ipm2011ecc_ed/AF591/11 | matthews2011ecc2 | EDIN-TAU-WDS | 73.487 | 0.257 | 13.719 | 3.485 | 0.136 | 0.142 | 1.204 | 4.769 | 3.483 | 0.032 | 0.162 | 0.191 | 101.076 | 1 | ||
| ipm2011ecc_ed/AF591/12 | matthews2011ecc2 | EDIN-TAU-WDS | 70.671 | 0.273 | 13.092 | 3.564 | 0.15 | 0.208 | 1.278 | 4.865 | 3.475 | 0.037 | 0.17 | 0.191 | 97.999 | 1 | ||
| ipm2011ecc_ed/AF591/13 | matthews2011ecc2 | EDIN-TAU-WDS | 70.472 | 0.27 | 12.693 | 3.48 | 0.14 | 0.205 | 1.214 | 5.136 | 3.357 | 0.035 | 0.163 | 0.191 | 97.367 | 1 | ||
| ipm2011ecc_ed/AF591/14 | matthews2011ecc2 | EDIN-TAU-WDS | 69.76 | 0.287 | 12.649 | 3.594 | 0.146 | 0.168 | 1.32 | 4.904 | 3.389 | 0.037 | 0.172 | 0.208 | 96.657 | 1 | ||
| ipm2011ecc_ed/AF591/15 | matthews2011ecc2 | EDIN-TAU-WDS | 69.753 | 0.283 | 12.81 | 3.307 | 0.135 | 0.186 | 1.254 | 4.776 | 3.36 | 0.037 | 0.168 | 0.17 | 96.25 | 1 |
| z | z_range | t | t_sigma | sample | volc_region | volcano | eruption | ref | ||
|---|---|---|---|---|---|---|---|---|---|---|
| -9544.5 | 295 | AF555-556 | EVZ | Katla | AF555 | doi:10.1002/jqs.1498 |
| labcode | batch | instrument | SiO2 | TiO2 | Al2O3 | FeOt | MnO | MgO | CaO | Na2O | K2O | P2O5 | Cl | F | total | ok | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| QUEST420/121/01 | QUEST-20 | QUEST-WDS | 73.86 | 0.3 | 11.93 | 2.53 | 0.08 | 0.25 | 1.54 | 3.32 | 2.45 | 0 | 0 | 0 | 96.27 | 1 | ||
| QUEST420/121/02 | QUEST-20 | QUEST-WDS | 72.93 | 0.33 | 11.76 | 2.5 | 0.07 | 0.27 | 1.57 | 3.44 | 2.48 | 0 | 0 | 0 | 95.35 | 1 | ||
| QUEST420/121/03 | QUEST-20 | QUEST-WDS | 74.04 | 0.31 | 11.88 | 2.45 | 0.09 | 0.27 | 1.65 | 3.2 | 2.47 | 0 | 0 | 0 | 96.36 | 1 | ||
| QUEST420/121/04 | QUEST-20 | QUEST-WDS | 75.01 | 0.29 | 12.03 | 2.55 | 0.09 | 0.26 | 1.57 | 2.89 | 2.55 | 0 | 0 | 0 | 97.24 | 1 | ||
| QUEST420/121/05 | QUEST-20 | QUEST-WDS | 75.05 | 0.31 | 12.23 | 2.54 | 0.08 | 0.25 | 1.63 | 3.08 | 2.51 | 0 | 0 | 0 | 97.67 | 1 |
| labcode | batch | instrument | SiO2 | TiO2 | Al2O3 | FeOt | MnO | MgO | CaO | Na2O | K2O | P2O5 | Cl | F | total | ok | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| QUEST420/122/01 | QUEST-20 | QUEST-WDS | 74.22 | 0.07 | 11.8 | 1.21 | 0.02 | 0.03 | 0.52 | 3.49 | 3.96 | 0 | 0 | 0 | 95.31 | 1 | ||
| QUEST420/122/02 | QUEST-20 | QUEST-WDS | 74.86 | 0.11 | 11.63 | 1.05 | 0.02 | 0.04 | 0.39 | 3.12 | 4.04 | 0 | 0 | 0 | 95.26 | 1 | ||
| QUEST420/122/03 | QUEST-20 | QUEST-WDS | 74.73 | 0.09 | 11.6 | 0.96 | 0.03 | 0.04 | 0.4 | 3.04 | 4.26 | 0 | 0 | 0 | 95.15 | 1 | ||
| QUEST420/122/04 | QUEST-20 | QUEST-WDS | 74.23 | 0.11 | 11.6 | 1.11 | 0.05 | 0.05 | 0.46 | 3.2 | 3.7 | 0 | 0 | 0 | 94.51 | 1 | ||
| QUEST420/122/05 | QUEST-20 | QUEST-WDS | 73.95 | 0.11 | 11.79 | 1.13 | 0.01 | 0.06 | 0.47 | 3.12 | 4.06 | 0 | 0 | 0 | 94.7 | 1 | ||
| QUEST420/122/06 | QUEST-20 | QUEST-WDS | 73.8 | 0.11 | 11.8 | 1.16 | 0.03 | 0.05 | 0.47 | 3.24 | 3.83 | 0 | 0 | 0 | 94.5 | 1 | ||
| QUEST420/122/07 | QUEST-20 | QUEST-WDS | 74.39 | 0.1 | 11.62 | 0.98 | 0.01 | 0.01 | 0.43 | 2.77 | 4.07 | 0 | 0 | 0 | 94.38 | 1 | ||
| QUEST420/122/08 | QUEST-20 | QUEST-WDS | 73.48 | 0.1 | 11.77 | 1.29 | 0.05 | 0.02 | 0.54 | 3.22 | 3.74 | 0 | 0 | 0 | 94.22 | 1 | ||
| QUEST420/122/09 | QUEST-20 | QUEST-WDS | 73.51 | 0.09 | 11.84 | 1.21 | 0.03 | 0.02 | 0.55 | 3.24 | 3.67 | 0 | 0 | 0 | 94.16 | 1 | ||
| QUEST420/122/10 | QUEST-20 | QUEST-WDS | 73.32 | 0.08 | 11.74 | 1.12 | 0.05 | 0.03 | 0.5 | 3.39 | 3.97 | 0 | 0 | 0 | 94.18 | 1 |
| labcode | batch | instrument | SiO2 | TiO2 | Al2O3 | FeOt | MnO | MgO | CaO | Na2O | K2O | P2O5 | Cl | F | total | ok | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| QUEST420/136/01 | QUEST-20 | QUEST-WDS | 73.57 | 0.14 | 12.39 | 1.47 | 0.04 | 0.04 | 0.72 | 3.39 | 3.99 | 0 | 0 | 0 | 95.75 | 1 | ||
| QUEST420/136/02 | QUEST-20 | QUEST-WDS | 73.11 | 0.13 | 12.3 | 1.52 | 0 | 0.07 | 0.77 | 3.62 | 3.68 | 0 | 0 | 0 | 95.2 | 1 | ||
| QUEST420/136/03 | QUEST-20 | QUEST-WDS | 73.02 | 0.14 | 12.38 | 1.59 | 0.05 | 0.07 | 0.66 | 3.47 | 3.8 | 0 | 0 | 0 | 95.18 | 1 | ||
| QUEST420/136/04 | QUEST-20 | QUEST-WDS | 72.9 | 0.14 | 12.3 | 1.5 | 0.04 | 0.09 | 0.72 | 3.37 | 3.9 | 0 | 0 | 0 | 94.96 | 1 | ||
| QUEST420/136/05 | QUEST-20 | QUEST-WDS | 73.18 | 0.07 | 12.27 | 1.5 | 0.03 | 0.09 | 0.77 | 3.26 | 3.76 | 0 | 0 | 0 | 94.93 | 1 | ||
| QUEST420/136/06 | QUEST-20 | QUEST-WDS | 72.99 | 0.14 | 12.36 | 1.51 | 0.02 | 0.09 | 0.79 | 3.38 | 3.63 | 0 | 0 | 0 | 94.91 | 1 | ||
| QUEST420/136/07 | QUEST-20 | QUEST-WDS | 73.12 | 0.1 | 12.23 | 1.57 | 0.03 | 0.09 | 0.72 | 3.25 | 3.72 | 0 | 0 | 0 | 94.83 | 1 | ||
| QUEST420/136/08 | QUEST-20 | QUEST-WDS | 72.87 | 0.11 | 12.47 | 1.51 | 0.05 | 0.08 | 0.74 | 3.29 | 3.69 | 0 | 0 | 0 | 94.81 | 1 | ||
| QUEST420/136/09 | QUEST-20 | QUEST-WDS | 72.64 | 0.13 | 12.28 | 1.61 | 0 | 0.11 | 0.83 | 3.53 | 3.68 | 0 | 0 | 0 | 94.81 | 1 | ||
| QUEST420/136/10 | QUEST-20 | QUEST-WDS | 73.12 | 0.1 | 12.19 | 1.4 | 0.07 | 0.06 | 0.68 | 3.31 | 3.83 | 0 | 0 | 0 | 94.75 | 1 | ||
| QUEST420/136/11 | QUEST-20 | QUEST-WDS | 72.93 | 0.13 | 12.22 | 1.53 | 0.06 | 0.08 | 0.74 | 3.37 | 3.68 | 0 | 0 | 0 | 94.74 | 1 | ||
| QUEST420/136/12 | QUEST-20 | QUEST-WDS | 72.76 | 0.18 | 12.18 | 1.5 | 0.03 | 0.1 | 0.77 | 3.36 | 3.86 | 0 | 0 | 0 | 94.74 | 1 | ||
| QUEST420/136/13 | QUEST-20 | QUEST-WDS | 72.72 | 0.11 | 11.98 | 1.5 | 0.06 | 0.1 | 0.74 | 3.66 | 3.87 | 0 | 0 | 0 | 94.74 | 1 | ||
| QUEST420/136/14 | QUEST-20 | QUEST-WDS | 72.91 | 0.12 | 12.09 | 1.35 | 0.05 | 0.05 | 0.83 | 3.38 | 3.92 | 0 | 0 | 0 | 94.7 | 1 | ||
| QUEST420/136/15 | QUEST-20 | QUEST-WDS | 72.86 | 0.13 | 12.29 | 1.49 | 0.05 | 0.05 | 0.77 | 3.36 | 3.69 | 0 | 0 | 0 | 94.69 | 1 | ||
| QUEST420/136/16 | QUEST-20 | QUEST-WDS | 72.77 | 0.11 | 12.29 | 1.51 | 0.07 | 0.12 | 0.74 | 3.41 | 3.66 | 0 | 0 | 0 | 94.68 | 1 | ||
| QUEST420/136/17 | QUEST-20 | QUEST-WDS | 72.6 | 0.13 | 12.34 | 1.47 | 0.06 | 0.07 | 0.84 | 3.46 | 3.68 | 0 | 0 | 0 | 94.63 | 1 | ||
| QUEST420/136/18 | QUEST-20 | QUEST-WDS | 73.03 | 0.11 | 12.24 | 1.48 | 0.05 | 0.06 | 0.76 | 3.3 | 3.57 | 0 | 0 | 0 | 94.58 | 1 | ||
| QUEST420/136/19 | QUEST-20 | QUEST-WDS | 72.69 | 0.17 | 12.12 | 1.5 | 0 | 0.11 | 0.9 | 3.38 | 3.67 | 0 | 0 | 0 | 94.54 | 1 | ||
| QUEST420/136/20 | QUEST-20 | QUEST-WDS | 72.98 | 0.16 | 12.39 | 1.18 | 0.04 | 0.08 | 0.62 | 3.4 | 3.67 | 0 | 0 | 0 | 94.52 | 1 | ||
| QUEST420/136/21 | QUEST-20 | QUEST-WDS | 73.08 | 0.11 | 12.25 | 1.09 | 0.02 | 0.03 | 0.7 | 3.31 | 3.78 | 0 | 0 | 0 | 94.37 | 1 | ||
| QUEST420/136/22 | QUEST-20 | QUEST-WDS | 72.61 | 0.13 | 12.27 | 1.48 | 0.05 | 0.08 | 0.76 | 3.24 | 3.74 | 0 | 0 | 0 | 94.34 | 1 | ||
| QUEST420/136/23 | QUEST-20 | QUEST-WDS | 72.34 | 0.13 | 12.32 | 1.49 | 0.02 | 0.09 | 0.7 | 3.23 | 3.82 | 0 | 0 | 0 | 94.14 | 1 |
| z | z_range | t | t_sigma | sample | volc_region | volcano | eruption | ref | ||
|---|---|---|---|---|---|---|---|---|---|---|
| -8859.5 | 240 | QUEST420/121 | NVZ | Askja | Askja-S | doi:10.1016/s0033-5894(03)00035-8 | ||||
| -9437.5 | 156 | QUEST420/122 | SVB | Snaefellsjokull | Hasseldalen tephra | doi:10.1016/s0033-5894(03)00035-8 |
| eruption | eruption_type | t | t_sigma | t_source | ref | notes | ||
|---|---|---|---|---|---|---|---|---|
| PMG-5 | Plinian | 1600.5 | 100 | doi:10.1191/0959683602hl538rr | possibly c. AD 1600 interpolated (Hall & Pilcher 2002). | |||
| BIP-24 | Plinian | 900.5 | 100 | doi:10.1111/j.1502-3885.2005.tb01011.x | c. AD 900 interpolated | |||
| AD860 Layer part B | Plinian | 860.5 | 20 | doi:10.1177/095968369500500111 | c. AD 860 ± 20 radiocarbon wiggle-match at Sluggan (AD lower layer, colourless tephra shards, two populations) | |||
| OMH-185 (Barnsmore) | Plinian | -716.5 | 38 | IntCal04 | doi:10.1191/0959683604hl757rr | c. 755-680 cal BC (Plunkett et al. 2004). According to Hall and Pilcher (2002) this is probably equivalent to the DOM-6 'microlite' tephra in Germany. | ||
| Derrycunihy Wood SH-1 | Plinian | |||||||
| FMAZ II (Fugloyarbanki) | Plinian | -24739.5 | 1 | GICC05 | doi:10.1002/jqs.1182 | 26740 ± 390 yr b2k in NGRIP 1848.05 | ||
| Borrobol | Plinian | -12094.5 | 95 | IntCal09 | doi:10.1002/jqs.1498 | Best current estimate is 14.14-13.95 cal ka BP (Bayesian age model). Replaces Turney et al. (1997) date of c.14.4 cal ka BP. Davies et al. (2004) suggestion of 2 eruptions has been revised by Matthews et al. (2011). | ||
| L3574 | Plinian | No age given, reported as 'older than Saksunarvatn tephra' by Dugmore and Newton (1997). Turney et al. (2006) suggests an age of c. 10.8 ka cal. BP. | ||||||
| OWB-105 AD700 | Plinian | 700.5 | 100 | doi:10.1191/0959683602hl538rr | c. AD 700 interpolated (Hall & Pilcher 2002). | |||
| Penifiler Tephra | Plinian | -11929.5 | 200 | IntCal09 | doi:10.1002/jqs.1498 | 14.08-13.68 cal ka BP (Bayesian age model) | ||
| Sluggan A | Plinian | -12549.5 | 500 | doi:10.1002/jqs.990 | c. 14500 cal BP suggested by Turney et al. (2006) | |||
| Sluggan B | Plinian | -10849.5 | 500 | doi:10.1002/jqs.990 | c. 12800 cal BP suggested by Turney et al. (2006) | |||
| AD860 Layer part A | Plinian | 860.5 | 20 | doi:10.1177/095968369500500111 | c. AD 860 ± 20 radiocarbon wiggle-match at Sluggan (AD lower layer, colourless tephra shards, two populations) | |||
| BMR-90 AD920 | Plinian | 920.5 | 100 | doi:10.1191/0959683602hl538rr | c. AD 920 interpolated (Hall & Pilcher 2002) | |||
| Breakish Tephra | Plinian | doi:10.1002/jqs.1066 | no date suggested although position above the Ashik tephra and Saksunarvatn indicates an age in the early-mid Holocene. | |||||
| DOM-6 'microlite' tephra | Plinian | -696.5 | 35 | doi:10.1006/qres.2002.2325 | c. 730-664 cal BC radiocarbon (van den Bogaard et al. 2002). According to Hall & Pilcher (2002) this is probably equivalent to the OMH-185 (Barnsmore) tephra. | |||
| GB4-182 | Plinian | -1349.5 | 200 | doi:10.1191/0959683602hl538rr | c. 1350 cal BC interpolated (Hall & Pilcher 2002) | |||
| GB4-50 AD1250 | Plinian | 1250.5 | 100 | doi:10.1191/0959683602hl538rr | c. AD 1250 interpolated (Hall & Pilcher 2002) | |||
| Harthorpe Moss tephra | Plinian | doi:10.1177/095968369600600112 | ||||||
| Lough Portain B | Plinian | 0 | doi:10.1177/095968369500500301 | sub-population of Hekla AD 1510 eruption (Lough Portain A). Status is unclear, not a distinct isochrone | ||||
| MOR-T4 | Plinian | 1000.5 | 100 | doi:10.1191/0959683604hl749rp | c. cal AD 1000 interpolated (Chambers et al. 2004) | |||
| Roddans Port A | Plinian | doi:10.1002/jqs.990 | two sub-populations (A & B) at 63-64 cm depth, dating unclear, pre-Vedde Ash. | |||||
| Roddans Port B | Plinian | doi:10.1002/jqs.990 | two sub-populations (A & B) at 63-64 cm depth, dating unclear, pre-Vedde Ash. | |||||
| SLU-5 | Plinian | 1650.5 | 50 | doi:10.1191/0959683602hl538rr | c. AD 1600-1700 interpolated (Hall & Pilcher 2002) | |||
| Stomyren tephra | Plinian | -149.5 | 100 | doi:10.1016/j.quaint.2004.04.030 | c. 2100 cal yr BP interpolated (Wastegard 2005) | |||
| Vallensgard Mose tephra | Plinian | doi:10.1002/jqs.990 | Stratigraphic position is similar to Vedde Ash, in the middle of the Younger Dryas, but geochemistry is different. Unclear if this is a significant tephra horizon. | |||||
| NAAZ I | Plinian | -10449.5 | 500 | Marine04 | doi:10.1016/j.quascirev.2006.03.001 | Diffuse layer representing c. 11 ka 14C yr GS-1 ash zone containing components from I-Thol-2 (Grímsvötn), I-Rhy.1 (Katla) and I-Thol-1 (Veidivötn). It is commonly believed that the biggest contributor is the rhyolitic component of the Vedde Ash. | ||
| L-274 | Plinian | -8274.5 | 100 | IntCal09 | doi:10.1016/j.quaint.2011.05.014 | 14C modeled age of 10,325-10,125 yr cal BP (Lind & Wastegard 2011). | ||
| 5d-BAS | Plinian | -109549.5 | 5000 | Orbital | doi:10.1016/s0277-3791(98)00038-9 | Probably represents an eruption complex. Several geochemical populations: BAS-I, BAS-II, BAS-III. | ||
| 5e-Midt | Plinian | -123049.5 | 5000 | Orbital | doi:10.1016/s0277-3791(98)00038-9 | Probably represents an eruption complex. Several geochemical populations: RHY, INT, BAS & TAB (the 5e-Midt/TRACHY is believed to be from Jan Mayen). Wallrabe-Adams & Lackschewitz (2002) suggest either Vatnafjoll or Vestmannaeyjar may be the source. | ||
| 5e-Low | Plinian | -127549.5 | 5000 | Orbital | doi:10.1016/s0277-3791(98)00038-9 | Probably represents an eruption complex. Several geochemical populations. Wallrabe-Adams & Lackschewitz (2002) suggest either Vatnafjoll or Vestmannaeyjar may be the source. | ||
| St. 5a-THOL-1 | Plinian | -74549.5 | 5000 | Orbital | doi:10.1016/0012-821x(95)00145-3 | THOL geochemical composition | ||
| St. 7-RHY-I & II | Plinian | -208049.5 | 20000 | Orbital | doi:10.1002/jqs.3390060205 | RHY-I & RHY-II geochemical compositions | ||
| St. 7-BAS/INT-I | Plinian | -208549.5 | 20000 | Orbital | doi:10.1002/jqs.3390060205 | INT-I & INT/BAS-I geochemical compositions | ||
| St. 9-RHY-I | Plinian | -328049.5 | 30000 | Orbital | doi:10.1002/jqs.3390060205 | RHY geochemical composition; possible equivalent to NAAZ III (III-RHY-I, c.320 ka) | ||
| St. 9-BAS-I | Plinian | -328049.5 | 30000 | Orbital | doi:10.1002/jqs.3390060205 | BAS geochemcial composition |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Ballysculllian East | UK | -6.462999821 | 54.79750061 | 44 | Terrestrial | QUEST621/111 | distal | fall | ash | quest | |||||
| Borg Indrepollen | Norway | 13.49400043 | 68.14499664 | Terrestrial | QUEST636/111 | distal | fall | ash | quest |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Borg Indrepollen | Norway | 13.49400043 | 68.14499664 | Terrestrial | QUEST636/110 | distal | fall | ash | quest |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Derrycunihy Wood | Ireland | -9.416669846 | 52.01670074 | Terrestrial | QUEST580/113 | distal | fall | ash | quest |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| K708-1 | -23.75 | 50 | -4053 | Marine | QUEST709/3 | distal | fall | ash | quest |
| eruption | eruption_type | t | t_sigma | t_source | ref | notes | ||
|---|---|---|---|---|---|---|---|---|
| Vedde Ash | Ultra-Plinian | -10170.5 | 1 | GICC05 | doi:10.1029/2005jd006079 | Bi-model rhyolitic and basalt ash layer, c. 12171 ± 114 yr b2k (GICC05); alternatively NGRIP SS09 11985-11988 ice core yr BP. Norddahl and Haflidason (1992) have suggested that the Skogar tephra is the proximal correlate of the Vedde Ash. | ||
| Katla AD1625 | Plinian | 1625.5 | 1 | Calendar | AD 1625 historical | |||
| Eldgja tephra | Sub-Plinian | 934.5 | 1 | GICC05 | doi:10.1177/095968369500500201 | c. AD 938 ± 4 (GISP2) or AD934 ± 2. Katla~1000 and K-x are now believed to correspond to this eruption (G. Larsen, 2010, Katla: tephrochronology and eruption history, in Schomacker et al. [eds.] 'The Mýrdalsjökull Ice Cap, Iceland: glacial processes, sediments and landforms on an active volcano', Developments in Quaternary Science vol. 13, pp.23-49, Amsterdam: Elsevier). | ||
| GA4-85 | Plinian | 750.5 | 50 | doi:10.1191/0959683602hl538rr | c. AD 700-800 interpolated (Hall & Pilcher 2002). | |||
| Tjornuvik AD800 B | Plinian | 800.5 | 50 | doi:10.1191/095968301668079904 | ninth century AD age suggested by Wastegard et al. (2001). | |||
| GB4-150 | Plinian | -777.5 | 21 | IntCal04 | doi:10.1191/0959683604hl757rr | c. 800-758 cal BC (Plunkett et al. 2004). | ||
| Mjauvotn A | Plinian | -4399.5 | 200 | doi:10.1191/095968301668079904 | c. 5300-5700 14C yr BP radiocarbon. A mid-distal basaltic tephra (Tv-5) dated to c. 6000 BP with a similar geochemistry to this tephra has been recorded in the sediment succession from Lake Torfadalsvatn on northern Iceland (Bjorck et al., 1992). | |||
| Mjauvotn B | Plinian | -4399.5 | 200 | doi:10.1191/095968301668079904 | c. 5300-5700 14C yr BP radiocarbon | |||
| Torfadalsvatn (Tv-5) | Sub-Plinian | -4954.5 | 240 | IntCal09 | doi:10.1111/j.1502-3885.1992.tb00009.x | Transitional alkali basalt. Dated at Lake Torfadalsvatn to 6000 ± 140 14C yr BP (c.7240-6500 cal BP, 2 sigma). Possibly the mid-distal equivalent of Mjauvotn A tephra on the Faroes (Wastegard 2001). On the basis of major element geochemistry believed to be from Katla. | ||
| SILK-A1 | Sub-Plinian | -4009.5 | 207 | IntCal09 | doi:10.1002/jqs.724 | c. 5170 ± 85 14C yr BP (Wastegard 2002, JQS 17(8), 723-730). Calibrates to 6182-5730 yr cal BP (2 sigma). | ||
| SILK-A7 | Sub-Plinian | -5189.5 | 123 | IntCal09 | doi:10.1002/jqs.724 | c. 6245 ± 90 14C yr BP calibrates to 7415-6932 yr cal BP (2 sigma; Wastegard 2002) | ||
| SILK-YN | Sub-Plinian | 310.5 | 70 | IntCal09 | doi:10.1179/env.2000.5.1.21 | There are three 14C ages for this tephra, from 1500 ± 70 to 1880 ± 60 14C yr BP. Dugmore et al. (2000) argue for an age of 1740 ± 50 14C yr BP. Calibrated age range of 1811-1539 cal BP (2 sigma). | ||
| Suduroy tephra | Plinian | -6119.5 | 90 | IntCal09 | doi:10.1002/jqs.724 | Rhyolitic ash layer, c. 7240 ± 95 14C yr BP calibrates to 8310-7868 cal BP (2 sigma; Wastegard 2002, JQS 17(8), 723-730). | ||
| NGRIP 1508.26m | Sub-Plinian | -10249.5 | 1 | GICC05 | doi:10.1029/2005jd006079 | Rhyolitic ash layer. NGRIP GICC05 age of 12250 ± 117 b2k years | ||
| NGRIP 1573.00m | Sub-Plinian | -12019.5 | 1 | GICC05 | doi:10.1029/2005jd006079 | Basalt layer. NGRIP GICC05 14020 ± 167 b2k. | ||
| Dimna Ash | Plinian | -13149.5 | 300 | IntCal04 | doi:10.1016/j.quascirev.2007.04.021 | Rhyolitic ash that is below radiocarbon age of 12780 ± 60 14C yr BP (15400-14850 cal BP) on terrestrial plant macrofossils (Koren et al. 2008) | ||
| AF555 | Plinian | -9544.5 | 295 | IntCal09 | doi:10.1002/jqs.1498 | Rhyolitic ash layer. Bayesian age model 11.79-11.20 cal ka BP | ||
| Solheimar Ignimbrite | Phreato-Plinian | -10149.5 | 700 | doi:10.1007/bf00298704 | correlated with Vedde Ash and dated to Younger Dryas Stadial. | |||
| NGRIP 1861.55m | Sub-Plinian | -25526.5 | 1 | GICC05 | doi:10.1016/j.epsl.2010.03.004 | Transitional alkali basalt; GICC05 age of 27527 ± 410 b2k | ||
| NGRIP 1895.24m | Sub-Plinian | -27129.5 | 1 | GICC05 | doi:10.1016/j.epsl.2010.03.004 | Transitional alkali basalt; GICC05 age of 29130 ± 456 b2k | ||
| IA2 | Sub-Plinian | -11199.5 | 146 | Orbital | doi:10.1016/s0277-3791(00)00146-3 | Ice rafted rhyolitic ash layer, Bond et al. (2001) assigns this to GI-1b which has a GICC05 age range of 13311-13099 b2k (± 146). | ||
| Skopun tephra | Plinian | -7799.5 | 100 | IntCal09 | doi:10.1016/j.quaint.2011.05.014 | 14C modeled age of 9850-9650 yr cal BP (Lind & Wastegard 2011). | ||
| St. 5a-TAB-1 | Plinian | -73449.5 | 5000 | Orbital | doi:10.1016/0012-821x(95)00145-3 | TAB geochemical composition | ||
| St. 5a-TAB-2 | Plinian | -75549.5 | 5000 | Orbital | doi:10.1016/0012-821x(95)00145-3 | TAB geochemical composition |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Borg Indrepollen | Norway | 13.49400043 | 68.14499664 | Terrestrial | QUEST636/54 | distal | fall | ash | quest |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Gurskøy | Norway | 5.557889938 | 62.3708992 | Terrestrial | QUEST637/3 | distal | fall | ash | quest | ||||||
| Kvaltjern | Norway | 4.981400013 | 60.42309952 | Terrestrial | QUEST639/3 | distal | fall | ash | quest | ||||||
| Lake Kullatorpssjön | Sweden | 12.48770046 | 56.29410172 | 89 | Terrestrial | QUEST692/3 | distal | fall | ash | quest | |||||
| Lake Mullsjön | Sweden | 14.36079979 | 58.36930084 | 133 | Terrestrial | QUEST695/3 | distal | fall | ash | quest | |||||
| Lerstadvatn, Ålesond | Norway | 6.260990143 | 62.36729813 | Terrestrial | QUEST641/3 | distal | fall | ash | quest | ||||||
| Lake Gjølvatn | Norway | 6.252160072 | 62.43230057 | Terrestrial | QUEST640/3 | distal | fall | ash | quest | ||||||
| Lillerestjønn | Norway | 6.31704998 | 62.46889877 | Terrestrial | QUEST642/3 | distal | fall | ash | quest | ||||||
| Saudedalsmyra | Norway | 6.236690044 | 62.43389893 | Terrestrial | QUEST643/3 | distal | fall | ash | quest | ||||||
| Lac de Sewen | France | 6.897220135 | 47.81169891 | 500 | Terrestrial | QUEST823/3 | distal | fall | ash | quest |