1887
Volume 47 Number 6
  • E-ISSN: 1365-2478

Abstract

The multifold acquisition principle was applied to a borehole radar survey, performed in a granitic site (Grimsel Test Site, Switzerland). Two multifold coverage acquisitions (40‐fold and 20‐fold) were carried out in a subhorizontal borehole. Instrumental drifts (transmission time and sampling frequency fluctuations) were corrected in order to remove shifts observed on CMP gathers and to optimize velocity analysis and trace stacking. Computation of velocity spectra was adapted in order to take into account the features of the medium investigated (homogeneous velocity, various reflector orientations). The NMO velocities were then interpreted as angles between reflectors and the survey line. The processing, based on the computation of several constant velocity stacked sections performed with different NMO velocities, leads to better results than the standard DMO + NMO processing. The signal‐to‐noise ratio of the stacked profile is improved in comparison with the single‐fold section, which results from a standard acquisition. From a practical point of view, the implementation of a multifold radar survey within a borehole is difficult but a greater investigation range is obtained, more reflectors are detected and the mapping of geological discontinuities is improved.

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2001-12-24
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References

  1. CaiJ. & McMechanG.A.1995. Ray‐based synthesis of bistatic ground‐penetrating radar profiles. Geophysics60,8796.
    [Google Scholar]
  2. CarcioneJ.M.1996. Ground‐penetrating radar: wave theory and numerical simulation in lossy anisotropic media. Geophysics61,16641677.
    [Google Scholar]
  3. DavisJ.L. & AnnanA.P.1989. Ground‐penetrating radar for high‐resolution mapping of soil and rock stratigraphy. Geophysical Prospecting37,531551.
    [Google Scholar]
  4. FechnerT. & YaramanciU.1996. Influence of complex dielectric properties on the characteristics of radar reflections. European Journal of Environmental and Engineering Geophysics1,287301.
    [Google Scholar]
  5. FisherE., McMechanG.A., AnnanA.P.1992. Acquisition and processing of wide‐aperture ground‐penetrating radar data. Geophysics57,495504.
    [Google Scholar]
  6. GoodmanD.1994. Ground‐penetrating radar simulation in engineering and archaeology. Geophysics59,224232.
    [Google Scholar]
  7. GrasmueckM.1996. 3‐D ground‐penetrating radar applied to fracture imaging in gneiss. Geophysics61,10501064.
    [Google Scholar]
  8. GreavesR.J., LesmesD.P., LeeJ.M., ToksözM.N.1996. Velocity variations and water content estimated from multi‐offset, ground‐penetrating radar. Geophysics61,683695.
    [Google Scholar]
  9. HaleD.1984. Dip‐moveout by Fourier transform. Geophysics49,741757.
    [Google Scholar]
  10. HollenderF.1999. Interprétation de la distortion des signaux géoradar propagés et réfléchis — développement d'une tomographie par bandes de fréquence. PhD thesis, Institut National Polytechnique de Grenoble.
  11. HollenderF. & TillardS.1998. Modeling ground‐penetrating radar wave propagation and reflexion with the Jonscher parametrization. Geophysics49,19331942.
    [Google Scholar]
  12. KeusenH.R., GanguinJ., SchulerP., BulettiM.1989. Felslabor Grimsel, Geologie. NAGRA Technical Report No. 87‐14.
  13. MalagodiS., OrlandoL., PiroS.1994. Improvement of signal to noise ratio of GPR using CMP acquisition and data processing. 5th International Conference on GPR, Kitchener, Ontario, Canada, Proceedings, 689701.
  14. MaurerH. & GreenA.G.1997. Potential coordinate mislocations in crosshole tomography: result from the Grimsel test site. Geophysics62,16961709.
    [Google Scholar]
  15. McMechanG.A., GaynorG.C., SzerbiakR.B.1997. Use of ground‐penetrating radar for 3‐D sedimentological characterization of clastic reservoir analogs. Geophysics62,786796.
    [Google Scholar]
  16. PipanM., FinettiI., GaluppoP., GelettiR.1995. Multifold advanced GPR techniques — a case history from the Aquileia archaeological park. 57th EAGE conference, Glasgow, UK, Extended Abstract, C006.
  17. TillardS.1994. Radar experiments in isotropic and anisotropic geological formations (granite and schists). Geophysical Prospecting42,615636.
    [Google Scholar]
  18. TillardS. & DuboisJ.‐C.1995. Analysis of GPR data: wave propagation velocity determination. Journal of Applied Geophysics33,7791.
    [Google Scholar]
  19. TurnerG. & SigginsA.F.1994. Constant Q attenuation of subsurface radar pulses. Geophysics59,11921200.
    [Google Scholar]
  20. XiongZ. & TrippA.C.1997. Ground‐penetrating radar responses of dispersive models. Geophysics62,11271131.
    [Google Scholar]
  21. YilmazÖ.1987. Seismic Data Processing. Investigations in Geophysics No. 2. SEG.
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