Abstract
Rana track annealing model 2007, based on an Arrhenius approach, is significantly modified, including new assumptions, fitting parameters, and analysis, to yield a new phenomenological model for annealing of fission tracks in apatite. Construction and optimization of the new six parameter model have been described in detail. The model shows a hybrid behavior. In Arrhenius plot, for higher temperatures (laboratory data included), iso-annealing lines are curved while, for low temperatures (geological time scale), iso-annealing lines become parallel straight lines. This is a new feature for any such model and has produced promising results. C-axis projected lengths from laboratory experiments on Durango apatite are employed to find model parameters. KTB borehole fission-track data are added to build the temperature function that modifies the original equation. Partial annealing zone (PAZ), closure temperature (\(T_{\mathrm{C}}\)) and total annealing temperature (\(T_{\mathrm{A}}\)) were calculated and compared to geological benchmarks. The predictions of the present model agreed well with low and high temperature benchmarks. PAZ, \(T_{\mathrm{C}}\) and \(T_{\mathrm{A}}\) predictions were also compared to the Fanning Curvilinear Arrhenius model predictions, resulting in good agreement. The present model is flexible enough to be applied to other fission-track systems, like zircon, muscovite and titanite.
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This work has been funded by Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq), Brazil through the research grant #308192/2019-2. Authors are indebted to the three anonymous reviewers for their criticisms and suggestions that truly helped us improving the quality of our paper.
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Appendix: Changing Rana (2007) model format
Appendix: Changing Rana (2007) model format
Here we show how to change the model Eq. (2) from its original format to the format \(g(r)=f(t,T)\) that allow us to identify its behavior on the Arrhenius plot.
The model proposed by Rana (2007) is given by:
Passing \(\beta\) to the left side:
Exponentiating both sides and rearaging terms:
Applying the \(\ln\) to both sides:
Changing parameters to \(C_0 = -ln t_0\) ; \(C_{1p}=1\); \(C_{2p}= -E_{\mathrm{a}}/k\); \(C_4=1/\beta\), the model equation becomes:
Equation (17) is a Parallel Linear model in Arrhenius pseudo-space.
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Rana, M.A., Lixandrão Filho, A.L. & Guedes, S. A new phenomenological model for annealing of fission tracks in apatite: laboratory data fitting and geological benchmarking. Phys Chem Minerals 48, 21 (2021). https://doi.org/10.1007/s00269-021-01143-9
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DOI: https://doi.org/10.1007/s00269-021-01143-9