Quantitative Thermochronology presents a range of numerical modeling techniques to allow the physical implications of isotopic age data to be explored. The authors provide analytical, semi-analytical, and numerical solutions to the heat transfer equation in a range of tectonic settings and under varying boundary conditions. They illustrate their modeling approach with a large number of case studies. Programs on an accompanying website provide a means of solving the heat transport equation to predict the ages of rocks and compare them directly to geological data. Short tutorials are also included.
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