10.1594/PANGAEA.954967Wölfler, AndreasAndreasWölfler0000-0001-8083-8695Wolff, ReinhardReinhardWolff0000-0002-0294-4879Hampel, AndreaAndreaHampelHetzel, RalfRalfHetzel0000-0002-3412-6344Dunkl, IstvánIstvánDunkl0000-0001-8438-2867PANGAEA2023Event labelLatitude of eventLongitude of eventElevation of eventGrains, counted/analyzedFission-tracks, spontaneous, densityFission-tracks, spontaneousFission-tracks, induced, densityFission-tracks, inducedFission-tracks, dosimeter, densityFission-tracks, dosimeterProbability, chi-square testAge, mineralAge, mineral, standard deviationUraniumFission-track length, meanFission-track length, mean, standard deviationFission-track lengthFission-track, DparGeological sampleApatite fission-track analysisCalculatedAge, fission-trackcalculated, 1 sigmaDataset10.1594/PANGAEA.95497310.1016/S0016-7037(96)00193-710.1016/j.gca.2005.01.02410.1016/S0009-2541(83)80026-6375 data pointstext/tab-separated-valuesCreative Commons Attribution 4.0 InternationalThe data set includes the geographic position and elevation of the analyzed samples and the obtained apatite fission track ages. ρs (ρi) is the spontaneous (induced) track density (105 tracks/cm2); Ns (Ni) is the number of counted spontaneous (induced) tracks; ρd is the dosimeter track density (105 tracks/cm2); Nd is the number of tracks counted on the dosimeter; P(χ2) is the probability of obtaining Chi-square value (χ2) for n degrees of freedom (where n is the number of crystals minus 1); ages were calculated using the zeta calibration method (Hurford and Green, 1983), glass dosimeter IRMM540, and zeta values of 226±13 a/cm2 determined with the Durango apatite standard.13.567114.130446.005847.0506Gurktal Alps, Austria