1887

Abstract

Summary

Inclusion of shear-wave seismic studies in the characterization of reservoir analogues has a great potential to provide a more detailed understanding of changes in petrophysical properties and their direct impact on the seismic reflectivity. Presented in this study are mainly shear-wave shot records to illustrate the data quality and difficulties that can occur during acquisition, from two field sites in Denmark: (1) Stevns Klint, southeast Denmark,with numerous supplementary data and outcrops at a nearby cliff profiles and quarry walls. At Stevns Klint a 500 m long shear-wave data set was already acquired. (2) The Rørdal chalk quarry in Aalborg, northern Denmark, which offers the opportunity to sample plugs horizontally and vertically with a very close tie planned high-resolution seismic profiles. Stevns and Rørdal are characterized by different acquisition conditions. While measurements at Stevns were carried out on an asphalt road, Rørdal gives the opportunity to measure directly on the chalk surface. However, we show through examples how excavating machines in Rørdal can produce reflections similar to the ones produced by the source signal and, therefore, preclude data acquisition during ongoing quarrying.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201702105
2017-09-03
2024-04-19
Loading full text...

Full text loading...

References

  1. Anderskouv, K., T.Damholt, and F.Surlyk
    . “Late Maastrichtian chalk mounds, Stevns Klint, Denmark—combined physical and biogenic structures.” Sedimentary Geology200.1 (2007): 57–72.
    [Google Scholar]
  2. Beilecke, T., U.Polom, and S.Hoffmann
    . “Efficient high resolution subsurface shear wave reflection imaging in sealed urban environments.” Near Surface 2006-12th EAGE European Meeting of Environmental and Engineering Geophysics, 2006.
    [Google Scholar]
  3. DruivengaG., et al.
    “Transportabler Scherwellenvibrator.” Deutsches Patent-und Markenamt, Offenlegungsschrift DE103.27 (2011): 757.
    [Google Scholar]
  4. NielsenL., et al.
    “Integrated seismic analysis of the Chalk Group in eastern Denmark—Implications for estimates of maximum palaeo-burial in southwest Scandinavia.” Tectonophysics511.1 (2011): 14–26.
    [Google Scholar]
  5. Surlyk, F., T.Damholt, and M.Bjerager
    . Stevns Klint, Denmark: uppermost Maastrichtian chalk, Cretaceous-Tertiary boundary, and lower Danian bryozoan mound complex, Geological Society of Denmark, 2006.
    [Google Scholar]
  6. Surlyk, F. et al.
    “The cyclic Rørdal member- a new lithostratigraphic unit of chronostratigraphic and palaeoclimatic importance in the upper Maastrichtian of Denmark.” Bulletin of the Geological Society of Denmark58(2010): 89–98.
    [Google Scholar]
http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201702105
Loading
/content/papers/10.3997/2214-4609.201702105
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