Software Open Access
Evangelos Moulas;
Mark T Brandon
Here we provide two versions of KADMOS software (MATLAB and OCTAVE) together with an extensive documentation.
KADMOS is set of MATLAB routines that can be used to calculate the apparent 40K-40Ar (and the associated 40Ar-39Ar) ages as a function of a sample’s thermal history. KADMOS is originally written in MATLAB language and utilizes the Finite-Element Method (FEM) with grid refinement. The advantage of KADMOS is that it has been optimized for accuracy, performance and for maximum flexibility with respect to the modelled scenarios. KADMOS can be used to evaluate the apparent ages of various crystals and various geometries (planar, cylindrical & spherical) simultaneously
Please read the documentation first for further instructions.
Name | Size | |
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KADMOS_Documentation.pdf
md5:10fa0ade0e0122f9ad5d38210e90e4ba |
1.1 MB | Download |
KADMOS_MATLAB.zip
md5:9b07ff3ec60d871ae04a466cf7d863e2 |
6.8 kB | Download |
KADMOS_OCTAVE.zip
md5:c665e670a030baf0220eccb4a8eee552 |
7.9 kB | Download |
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McDougall, I., and Harrison, T. M., 1999, Geochronology and Thermochronology by the 40Ar/39Ar Method: Oxford University Press, 269 p
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Reiners, P. W., Carlson, R. W., Renne, P. R., Cooper, K. M., Granger, D. E., McLean, N. M., and Schoene, B., 2017, Diffusion and thermochronologic interpretations, in Geochronology and Thermochronology: John Wiley & Sons, Ltd, p. 83–126
Robbins, G. A., 1972, Radiogenic argon diffusion in muscovite under hydrothermal conditions
Simpson, G., 2017, Practical Finite Element Modelling in Earth Science Using Matlab: Wiley-Blackwell, 248 p
Skipton, D. R., Warren, C. J., and Hanke, F., 2018, Numerical models of P–T, time and grain-size controls on Ar diffusion in biotite: An aide to interpreting 40Ar/39Ar ages: Chemical Geology, v. 496, p. 14–24
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Data volume | 68.8 MB | 68.8 MB |
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