1887

Abstract

Summary

This contribution presents a new workflow for compaction analysis and top seal evaluation by wireline logging data. Sonic and density logs from nine key wells in the Vienna Basin (Austria), providing a continuous depth record from 0 to 3500 m true vertical depth (TVD), were filtered by natural gamma ray, resistivity, delta rho, and caliper to bit size, to identify mudstone intervals with reliable sonic and density signals. The calculated sonic- and density-porosity depth-trends were then quality-checked with core petrophysical data, e.g., helium-porosity and hydrocarbon column heights (HCHs) calculated based on true displacement radii from mercury intrusion capillary porosimetry (MICP). Furthermore, both porosity logs were corrected by their regressions with corresponding helium-porosity values from equal depths to obtain reliable log-based compaction models. Based on these models and the relationship between helium-porosity vs. HCH from MICP, log-based HCH vs. TVD curves were generated. In conclusion, both sonic- and density-porosity trends represent the core petrophysical data well. The HCH model based on density-porosity changed more significantly upon correction, after which both sonic- and density-based HCH trends plot similarly and allow for upscaling of the core petrophysical data to all wells with available wireline logs.

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/content/papers/10.3997/2214-4609.202335021
2023-11-27
2025-11-07
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References

  1. Arzmüller, G., Buchta, Š., Ralbovský, E. and Wessely, G. [2006] The Vienna Basin. In: Golonka, J. and Picha, F.J. (Eds.) The Carpathians and their foreland: Geology and hydrocarbon resources. American Association of Petroleum Geologists, Tulsa, Oklahoma, U.S.A.
    [Google Scholar]
  2. Bowers, G.L. [2002] Detecting high overpressure.The Leading Edge, 21(2), 174–177.
    [Google Scholar]
  3. Issler, D.R. [1992] A New Approach to Shale Compaction and Stratigraphic Restoration, Beaufort-Mackenzie Basin and Mackenzie Corridor, Northern Canada (1).AAPG Bulletin, 76.
    [Google Scholar]
  4. Misch, D., Siedl, W., Drews, M., Liu, B., Klaver, J., Pupp, M. and Sachsenhofer, R.F. [2021] Mineralogical, BIB-SEM and Petrophysical Data in Seal Rock Analysis: A Case Study from the Vienna Basin, Austria.Journal of Petroleum Geology, 44(1), 25–46.
    [Google Scholar]
  5. Raiga-Clemenceau, J., Martin, J.P. and Nicoletis, S. [1988] The concept of acoustic formation factor for 794 more accurate porosity determination from sonic transit time data.Log Anal, 29(1), 54–60.
    [Google Scholar]
  6. Skerbisch, L., Misch, D., Drews, M., Stollhofen, H., Sachsenhofer, R.F., Arnberger, K., Schuller, V. and Zamolyi, A. [2023] Regional mudstone compaction trends in the Vienna Basin: top seal assessment and implications for uplift history.International Journal of Earth Sciences.
    [Google Scholar]
  7. Yang, Y. and Aplin, A.C. [1998] Influence of lithology and compaction on the pore size distribution and modelled permeability of some mudstones from the Norwegian margin.Marine and Petroleum Geology, 15(2), 163–175.
    [Google Scholar]
  8. Yang, Y. and Aplin, A.C. [2004] Definition and practical application of mudstone porosity–effective stress relationships.Petroleum Geoscience, 10(2), 153–162.
    [Google Scholar]
  9. Yang, Y. and Aplin, A.C. [2010] A permeability–porosity relationship for mudstones.Marine and Petroleum Geology, 27(8), 1692–1697.
    [Google Scholar]
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