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Abstract

Summary

In this study we show how we can combine basin modeling principles with rock physics models. We apply the Walderhaug diagenetic modeling approach to simulate porosity and rock texture evolution during geological time, and use these as input to contact theory rock physics models which allows us to predict seismic properties as a function of the burial history. We also demonstrate how this approach can be used to estimate tectonic uplifts, and show an example from the Barents Sea.

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/content/papers/10.3997/2214-4609.20140659
2014-06-16
2024-04-19
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References

  1. Lander, R.H., and Walderhaug, O.
    , 1999, Predicting porosity through simulating sandstone compaction and quartz cementation; AAPG Bulletin, V.83, 433–449.
    [Google Scholar]
  2. Mavko, G., Dvorkin, J., and Mukerji, T.
    , 2009, The Rock Physics Handbook, Cambridge University Press.
    [Google Scholar]
  3. Walderhaug, O.
    , 1996, Kinetic modelling of quartz cementation and porosity loss in deeply buried sandstone reservoirs; AAPG Bulletin, V. 80, 731–745.
    [Google Scholar]
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