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than those with low values. For example, one data set might include only AFT data, a second AFT as well as AHe data, while a third might throw some vitrinite reflectance data into the mix as well. In conclusion, the evaluation of whether an inverse model is physically sound is more subjective in QTQt than it is in HeFTy. Hurford, Improved modeling of fission-track annealing in apatite, American Mineralogist 92 (5-6) (2007) 799810. Villa, From nanometer to megameter: Isotopes, atomic-scale processes and continent-scale tectonic models, Lithos 87 (2006) 155173.

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Furthermore, the sampling density of HeFTys randomly selected t-T paths also depends on the allowed range of time and temperature. In addition to the AFT data, we also measured five apatite U-Th-He (AHe) ages, ranging from 47-66. 23. . By using p-values, HeFTy contains a built-in quality control mechanism which can protect the user from the worst kinds of garbage data. A number of explanations have been proposed to explain this dispersion over the years, ranging from invisible and insoluble actinide-rich mineral inclusions ( 19 -implantation by bad neighbours ( 20 fragmentation during mineral separation ( 21 ) and radiation damage due to -recoil (. In fact, increasing the quantity (sample size) or quality (precision) of the data only has beneficial effects as it tightens the solution space (Figure 4 (iv). (iv) QTQtmakes a random walk (Markov Chain) through parameter space, sampling the posterior distribution and yielding an assemblage of best fitting slopes and intercepts (black dots and lines). HeFTy and QTQt are based on the same physical principles and their forward modelling functionalities are therefore nearly identical. Hu, A thermochronological perspective on the morphotectonic evolution of the southeastern Tibetan Plateau, Journal of Geophysical Research: Solid Earth.

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