Table 1
Sample details and results including sampling locality, WGS84 projection system coordinates, elevation, stratigraphic age and lithology.
Code | Locality | Lat | Long | Elevation (m) | Stratigraphic age (Ma) | Lithology | n | ρs | Ns | ρi | Ni | ρd | Nd | P (χ2) % ± 1 σ (Ma) | Central age | N | MTL ± 1SE (μm) | SD (μm) | Dpar± 1σ (μm) | Cl content Ox. Wt (%) |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
BEL1 | Fauquez | 50.626 | 4.218 | 85 | Ashgill | Dacite | 37 | 0.334 | 478 | 0.192 | 274 | 5.31 | 16140 | > 99 | 150 ± 12 | 12 | 13.3 ± 0.4 | 1.3 | 1.0 ± 0.1 | 0.2 |
BEL12 | Lessines | 50.713 | 3.867 | 35 | Lower Silurian | Porphyre | 14 | 0.553 | 213 | 0.242 | 93 | 5.31 | 16140 | > 99 | 195 ± 25 | 9 | 13.8 ± 0.3 | 0.9 | 1.2 ± 0.1 | |
BEL13 | Quenast | 50.665 | 4.160 | 28 | Caradoc | Porphyre | 24 | 0.467 | 342 | 0.281 | 206 | 5.23 | 16140 | > 99 | 140 ± 13 | 22 | 12.6 ± 0.2 | 1.1 | 1.1 ± 0.1 | |
BEL26 | Colfontaine | 50.385 | 3.845 | 121 | Lochkovian | Sandstone | 23 | 0.574 | 467 | 0.231 | 188 | 5.26 | 16140 | 97 | 209 ± 19 | – | – | – | 1.3 ± 0.1 | |
BEL27 | Sosoye | 50.300 | 4.795 | 190 | Visean | Ash-bed | 20 | 2.394 | 953 | 0.902 | 359 | 5.24 | 16140 | 99 | 223 ± 15 | 20 | 13.2 ± 0.3 | 1.3 | 1.5 ± 0.2 | |
BEL28 | Walhorn | 50.671 | 6.504 | 285 | Visean | Ash-bed | 31 | 2.043 | 1277 | 0.806 | 504 | 5.29 | 16140 | 49 | 213 ± 14 | 103 | 12.9 ± 0.1 | 1.4 | 1.6 ± 0.2 | |
BEL29 | Lives | 50.469 | 4.921 | 115 | Visean | Ash-bed | 9 | 1.907 | 225 | 0.881 | 104 | 5.43 | 16173 | > 99 | 188 ± 23 | – | – | – | 1.6 ± 0.1 | |
BEL30 | Saint-Servais | 50.478 | 4.853 | 140 | Visean | Ash-bed | 21 | 2.117 | 794 | 1.003 | 376 | 5.49 | 16140 | 64 | 186 ± 14 | 12 | 12.8 ± 0.1 | 1.8 | 1.2 ± 0.1 | |
BEL31 | Monceau-sur-Sambre | 50.398 | 4.379 | 120 | Visean | Ash-bed | 7 | 1.031 | 135 | 0.473 | 62 | 5.28 | 16140 | 28 | 181 ± 32 | – | – | – | 1.7 ± 0.2 | |
BEL32 | Maizeret | 50.464 | 4.999 | 105 | Visean | Ash-bed | 12 | 0.859 | 164 | 0.503 | 96 | 2.35 | 16140 | 59 | 147 ± 20 | – | – | – | 1.5 ± 0.2 | |
BEL33 | Royseux | 50.466 | 5.275 | 200 | Visean | Ash-bed | 34 | 2.4 | 1812 | 1.042 | 787 | 5.45 | 16140 | 56 | 201 ± 11 | 85 | 13.4 ± 0.1 | 1.2 | 1.4 ± 0.1 | |
BEL34 | Frasnière | 50.434 | 4.738 | 155 | Visean | Ash-bed | 22 | 0.821 | 482 | 0.296 | 174 | 5.56 | 16140 | > 99 | 246 ± 23 | 29 | 13.8 ± 0.2 | 0.9 | 1.7 ± 0.2 | 1.3 |
BEL35 | Anhée Nord | 50.317 | 4.876 | 105 | Visean | Ash-bed | 28 | 2.339 | 1097 | 0.761 | 357 | 5.27 | 16140 | 85 | 258 ± 18 | 24 | 13.7 ± 0.2 | 0.9 | 1.6 ± 0.1 | |
BEL36 | Anhée Sud | 50.294 | 4.894 | 115 | Visean | Ash-bed | 18 | 1.746 | 618 | 0.644 | 228 | 5.22 | 16140 | 54 | 226 ± 19 | 20 | 13.7 ± 0.2 | 0.9 | 2.2 ± 0.2 | 2.0 |
BEL37 | Landelies | 50.394 | 4.3368 | 120 | Visean | Ash-bed | 12 | 2.602 | 851 | 1.037 | 339 | 5.3 | 16140 | 77 | 213 ± 15 | 102 | 13.5 ± 0.1 | 1.1 | 1.3 ± 0.1 | |
BEL38 | Engihoul | 50.576 | 5.421 | 160 | Visean | Ash-bed | 30 | 2.982 | 2213 | 1.164 | 864 | 5.38 | 16140 | 14 | 196 ± 11 | 100 | 13.5 ± 0.2 | 1.5 | 1.6 ± 0.2 | 0.7 |
BEL39 | Seilles | 50.496 | 5.488 | 90 | Visean | Ash-bed | 23 | 1.957 | 1059 | 1.091 | 590 | 5.21 | 16140 | 69 | 152 ± 9 | 102 | 13.3 ± 0.1 | 1.2 | 1.6 ± 0.1 | 0.7 |
BEL41 | Anzin | 50.384 | 3.634 | −745 | Upper Carboniferous | Ash-bed | 24 | 1.153 | 534 | 0.847 | 392 | 5.17 | 16140 | 85 | 114 ± 8 | 10 | 13.4 ± 0.4 | 1.1 | 1.1 ± 0.1 | |
BEL49 | Couvin | 50.723 | 4.511 | 171 | Frasnian | Ash-bed | 21 | 0.62 | 264 | 0.197 | 84 | 5.2 | 16173 | 91 | 261 ± 33 | – | – | – | 1.3 ± 0.1 |
n: number of apatite crystals counted; s, i and d subscripts denote spontaneous, induced and dosimeter; ρ: track density (×105 tracks/cm2); N: number of tracks counted; P(χ2): probability of obtaining Chi-square value (χ2) for n degrees of freedom (where n = number of crystals – 1); Age ± 1σ – central age ± 1 standard error (Galbraith and Laslett, 1993); MTL: mean track length (μm); SD: standard deviation of track length distribution (μm); N(L): number of horizontal confined tracks measured; Dpar: average etch pit diameter parallel to c. Ages were calculated using the zeta calibration method (Hurford and Green, 1983), glass dosimeters CN-5, and a zeta value of 325 ± 4 (IB).
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