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Swiss Journal of Geosciences
Fig. 3 | Swiss Journal of Geosciences

Fig. 3

From: Tracing metamorphism, exhumation and topographic evolution in orogenic belts by multiple thermochronology: a case study from the Nízke Tatry Mts., Western Carpathians

Fig. 3

Thermal modelling results of thermochronological data displayed in a time–temperature diagram modelled with the HeFTy program (Ketcham, 2005). The best fit is shown as a solid black line, shaded polygons (yellow acceptable fit, blue good fit) show the values of peak temperatures after Eocene cooling and during post-Eocene reheating. ZHePRZ ZHe partial retention zone, APAZ apatite partial annealing zone, AHePRZ AHe partial retention zone, MTL mean track length in μm, SD standard deviation in μm, GOF goodness of fit (statistical comparison of the measured input data and modelled output data, where a “good” result corresponds to value 0.5 or higher, “best” result corresponds to value 1). Note that according to the modelling results, reheating could occur anytime from the Oligocene to the Late Miocene and thus is not in favour of any of the suggested geological scenarios

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