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The Use of Fission Track Measurements in Basin Modeling

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Part of the book series: Computer Applications in the Earth Sciences ((CAES))

Abstract

Forward modeling of fission track annealing of apatites is used together with basin modeling to estimate past heat flow and amount of erosion. For a known uranium concentration the track length histogram and the surface track density, hold information on the thermal history of the minerals. An equation is developed which is used to determine the number of horizontal (relative to prismatic faces) tracks in the histogram that has been generated after deposition. The post-sedimentary thermal history of the sample is calculated by a ID-basin model with an initial estimate on the paleoheat flow. The thermal history then is used to calculate the track length histogram including distribution of track lengths caused by distribution of energy of fission products and anisotropy. Adjustments of the paleoheat flow or the erosion depth are performed to obtain a better match between the calculated and measured track length histograms (post-sedimentary stage).The modeling is applied to the Danish North Sea well D-l.Fission track measurements on apatite are available at three depths.

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© 1993 Springer Science+Business Media New York

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Jensen, P.K., Bidstrup, T., Hansen, K., Kunzendorf, H. (1993). The Use of Fission Track Measurements in Basin Modeling. In: Harff, J., Merriam, D.F. (eds) Computerized Basin Analysis. Computer Applications in the Earth Sciences. Springer, Boston, MA. https://doi.org/10.1007/978-1-4615-2826-5_7

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  • DOI: https://doi.org/10.1007/978-1-4615-2826-5_7

  • Publisher Name: Springer, Boston, MA

  • Print ISBN: 978-1-4613-6222-7

  • Online ISBN: 978-1-4615-2826-5

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