1887

Abstract

Summary

Lithofacies types present a means to characterize subsurface facies from description of the sedimentological inventory. While sedimentary structures and grain size can be assessed in core and outcrop, dimensions and lateral extension are best observed in outcrops on the 10 to 100m-scale. Thus analogs are needed to map lithofacies types in 2D to 3D.

In our study we assess lithofacies types in a Lower Buntsandstein outcrop of the marginal facies in Southern Germany. The outcrop consists of wavy- and cross-bedded, subarkosic sandstones. Lithofacies types were cropping out in 3D and could be characterized macroscopically and with regard to mineral assemblage allowing to unravel the paragenetic sequence. Petrographic results were linked with porosity and permeability measured in plugs representing three spatial directions. Those revealed that flow directions play a subordinate role in the studied deposit, whereas lithofacies types coincide with markedly different petrophysical properties. The wavybedded lithofacies exhibited permeability ranges of 10-3 to 100 mD while the cross-bedded lithofacies type hosts permeabilities of 10-1 to 102 mD.

Our case study evidences how lithofacies type mapping in outcrop analogs offers an opportunity to construct and assign buildings blocks for fluid flow models that outdo permeability assessments from wireline logs and core descriptions.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.202021071
2020-11-16
2024-04-28
Loading full text...

Full text loading...

References

  1. Backhaus, E.
    , 1974. Limnische und fluviatile Sedimentation im südwestdeutschen Buntsandstein.Geologische Rundschau63, 925–942. https://doi.org/10.1007/BF01821318
    [Google Scholar]
  2. Becker, I., Wüstefeld, P., Koehrer, B., Felder, M., Hilgers, C.
    , 2017. Porosity and permeability variations in a tight gas sandstone reservoir analogue, Westphalian D, Lower Saxony Basin, NW Germany: Influence of depositional setting and diagenesis.Journal of Petroleum Geology40, 363–389. https://doi.org/10.1111/jpg.12685
    [Google Scholar]
  3. Busch, B., Hilgers, C., Gronen, L., Adelmann, D.
    , 2017. Cementation and structural diagenesis of fluvio-aeolian Rotliegend sandstones, northern England.Journal of the Geological Society174, 855–868. https://doi.org/10.1144/jgs2016-122
    [Google Scholar]
  4. Folk, R.L.
    , 1980. Petrology of sedimentary rocks.Hemphill Pub. Co, Austin, Texas.
    [Google Scholar]
  5. Günther, D.
    , 2010. Der Schwarzwald und seine Umgebung: Geologie, Mineralogie, Bergbau ; Umwelt und Geotourismus, Sammlung geologischer Führer. Borntraeger, Stuttgart.
    [Google Scholar]
  6. Klinkenberg, L.J.
    , 1941. The permeability of porous media to liquids and gases. Presented at the Drilling and Production Practice, American Petroleum Institute, New York.
    [Google Scholar]
  7. Leiber, J., Bock, H.
    , 2013. Der Buntsandstein in der Kraichgau-Senke und des südwestdeutschen Randfazies (Baden-Württemberg), in: Buntsandstein, Deutsche Stratigraphische Kommission (Hrsg.; Koordination und Redaktion: J. Lepper & H.-G. Röhling für die Subkommission Perm-Trias): Stratigraphie von Deutschland. Dt. Ges. Geowiss, Hannover, pp. 43–67.
    [Google Scholar]
  8. Lundegard, P.
    , D., 1992. Sandstone porosity loss - a “big picture” view of the importance of compaction.Journal of Sedimentary Petrology62, 250–260.
    [Google Scholar]
  9. Meyer, R., Krause, F.F.
    , 2006. Permeability anisotropy and heterogeneity of a sandstone reservoir: analogue: An estuarine to shoreface depositional system in the Virgelle Member, Milk River Formation, Writing-on-Stone Provincial Park, southern Alberta.Bulletin of Canadian Petroleum Geology54, 301–318.
    [Google Scholar]
  10. Miall, A.D.
    , 1996. The geology of fluvial deposits: sedimentary facies, basin analysis, and petroleum geology.Springer, Berlin ; New York.
    [Google Scholar]
  11. Paxton, S.T., Szabo, J.O., Ajdukiewicz, J.M., Klimentidis, R.E.
    , 2002. Construction of an intergranular volume compaction curve for evaluating and predicting compaction and porosity loss in rigid-grain sandstone reservoirs.AAPG Bulletin86, 2047–2067.
    [Google Scholar]
  12. Pranter, M.J., Ellison, A.I., Cole, R.D., Patterson, P.E.
    , 2007. Analysis and modeling of intermediate-scale reservoir heterogeneity based on a fluvial point-bar outcrop analog, Williams Fork Formation, Piceance Basin, Colorado.AAPG Bulletin91, 1025–1051. https://doi.org/10.1306/02010706102
    [Google Scholar]
  13. Reinecker, J., Grobe, R., Hochschild, T., Bauer, J., Meier, S., Philipp, S., Filomena, M., Stollhofen, H., Bechstädt, T., Drews, T., Miernik, G., Soyk, D., Melchert, B.
    , 2015. Verbundprojekt AuGE: Aufschlussanalogstudien und ihre Anwendbarkeit in der geothermischen Exploration -Entwicklung von Methoden zur Ermittlung von Permeabilitäten und Transmissivitäten aus Reservoir-Informationen des Oberrheingrabens (Schlussbericht Teilprojekt A), AuGE Outcrop Analogue Studies in Geothermal Exploration. GeoThermal Engineering GmbH, Karlsruhe.
    [Google Scholar]
  14. Rieckmann, M.
    , 1970. Untersuchung von Turbulenzerscheinungen beim Fließen von Gasen durch Speichergesteine unter Berücksichtigung der Gleitströmung.Erdoel-Erdgas-Zeitschrift86, 36–51.
    [Google Scholar]
  15. Röhling, H.-G., Lepper, J.
    , 2013. Paläogeographie des Mitteleuropäischen Beckens während der tieferen Trias (Buntsandstein), in: Buntsandstein, Deutsche Stratigraphische Kommission (Hrsg.; Koordination und Redaktion: J. Lepper & H.-G. Röhling für die Subkommission Perm-Trias): Stratigraphie von Deutschland. Dt. Ges. Geowiss, Hannover, pp. 43–67.
    [Google Scholar]
  16. Taylor, J.M.
    , 1950. Pore-space reduction in sandstones.AAPG Bulletin34, 701–716.
    [Google Scholar]
http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.202021071
Loading
/content/papers/10.3997/2214-4609.202021071
Loading

Data & Media loading...

This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error