1887
Volume 35, Issue 3
  • ISSN: 0812-3985
  • E-ISSN: 1834-7533

Abstract

The minimum size for shallow horizontal structures to be detectable and resolvable with airborne electromagnetic (AEM) systems is discussed, using synthetic modelling results and analysis of survey data.

Synthetic data were generated for the helicopter frequency-domain system RESOLVE and the fixed-wing time-domain systems TEMPEST and GEOTEM. The modelled scenarios include conductive prisms in a resistive host and resistive prisms in a conductive host. The EM responses of these models were computed for a range of prism thicknesses, side-lengths and host conductivities. Gaussian noise in amplitude comparable to actual system noise levels was added to the synthetic data followed by the derivation of conductivity-depth sections via three-layer inversion and EMFLOW conductivity-depth imaging. Where these ID algorithms failed to indicate the presence of the prism, the data were inspected for prism anomalies in order to evaluate whether 2D or 3D algorithms might be able to map these structures.

Results from the modelling of synthetic data indicate that beyond a minimum prism conductance (conductivity-thickness product), prism thickness is much less important for prism detectability than side-length. The minimum prism conductances determined for the RESOLVE, TEMPEST, and GEOTEM system are 1, 2, and 8 S, respectively. For horizontal prisms to be detectable with the RESOLVE system on response profiles and ID conductivity-depth sections they have to be at least 12 m wide. In order to resolve their thicknesses and conductivities, the prisms must be at least 120 m wide. For horizontal prisms to be detectable with the TEMPEST and GEOTEM system on ID conductivity-depth sections they have to be at least 150 m wide. In order to resolve their thicknesses and conductivities, the prisms must be at least 450 m wide. Profile inspection shows that horizontal structures as narrow as 24 m might be detectable with more advanced algorithms. However, the minimum size for resolving a prism‘s parameters is not a result of the application of ID algorithms but is defined by the system’s minimum footprint, which is a function of the system‘s geometry.

Some results of the synthetic data were confirmed by analysis of recent RESOLVE and TEMPEST survey data, which suggests conductive structures have to be at least 10-20 and 100-160 m wide, respectively, to be mapped on EMFLOW sections.

Loading

Article metrics loading...

/content/journals/10.1071/EG04208
2004-09-01
2026-01-16
Loading full text...

Full text loading...

References

  1. Green, A., 1998, Altitude correction of time domain AEM data for image display and geological mapping using the Apparent Dipole Depth (ADD) method: Exploration Geophysics, 29, 87-91.
  2. Green, A. A., and Lane, R. J.L., 2003, Estimating noise levels in AEM data: 16th Geophysical Conference and Exhibition, Australian Society of Exploration Geophysicists, Extended Abstracts.
  3. Lane, R., Plunkett, C., Price, A., Green A., and Hu, Y., 1998, Streamed data - a source of insight and improvement for time domain airborne EM: Exploration Geophysics, 29, 16-23.
  4. Lane, R., Green. A., Golding, C., Owers, M., Pik, P., Plunkett, C., Sattel, D., and Thorn, B., 2000, An example of 3D conductivity mapping using the TEMPEST AEM system: Exploration Geophysics, 31, 162-172.
  5. Liu, G. and Becker, A., 1990, Two-dimensional mapping of sea-ice keels with airborne electromagnetics: Geophysics, 55, 239-248.
  6. Macnae, L, King, A., Stolz, N., Osmakoff, A., and Blaha, A., 1998, Fast AEM data processing and inversion: Exploration Geophysics, 29, 163-169.
  7. Munday, T., Green, A., Brodie, R., Lane, R., Sattel, D., Cooke P., and Dodds S., 2003, Developing recharge reduction strategies in the Riverland of South Australia using AEM data, a case study in tailoring airborne geophysics given a particular target and a desired set of outcomes: 16th Geophysical Conference and Exhibition, Australian Society of Exploration Geophysicists, Extended Abstracts.
  8. Munday, T., and Walker, G., 2003, South Australian salt mapping and management support project - an example of the considered application of airborne geophysics in natural resource management: 16th Geophysical Conference and Exhibition, Australian Society of Exploration Geophysicists, Extended Abstracts.
  9. Raiche, A.P, 1997, MARCO-AIR, modelling program for sponsors of Australian Minerals Industry Research Association Project P223C.
  10. Reid, J. E., Vrbancich, J., and Worby, A.P, 2003, A comparison of shipborne and airborne electromagnetic methods for Antarctic sea ice thickness measurements: Exploration Geophysics, 34, 56-50.
  11. Reid, J. E., and Vrbancich, J., 2004, A comparison of the inductive-limit footprints of airborne electromagnetic systems: Geophysics (in press).
  12. Sattel, D., 1998, Conductivity information in three dimensions: Exploration Geophysics, 29, 157-162.
  13. Smith, B. D., Irvine, R., Blome, C, Clark, A., and Smith, D. V., 2003, Preliminary results, helicopter electromagnetic and magnetic survey of the Seco Creek area, Medina and Uvalde counties, Texas: Symposium on the Application of Geophysics to Engineering and Environmental Problems (SAGEEP) 2003, EEGS, 403-418.
  14. Smith, R. S., and Annan, A.P, 1997, Advances in airborne time-domain EM technology: in Gubins, A. G., (ed.), Proceedings of Exploration 97: Fourth Decennial International Conference on Mineral Exploration, 497-504.
  15. Munday, T., Green, A., Brodie, R., Lane, R., Sattel, D., Cooke R, and Dodds S., 2003, Developing recharge reduction strategies in the Riverland of South Australia using AEM data, a case study in tailoring airborne geophysics given a particular target and a desired set of outcomes: 16’h Geophysical Conference and Exhibition, Australian Society of Exploration Geophysicists, Extended Abstracts.
  16. Munday, T., and Walker, G., 2003, South Australian salt mapping and management support project - an example of the considered application of airborne geophysics in natural resource management: 16"1 Geophysical Conference and Exhibition, Australian Society of Exploration Geophysicists, Extended Abstracts.
  17. Raiche, A.R, 1997, MARCO-AIR, modelling program for sponsors of Australian Minerals Industry Research Association Project P223C.
  18. Reid, J. E., Vrbancich, J., and Worby, A. P., 2003, A comparison of shipborne and airborne electromagnetic methods for Antarctic sea ice thickness measurements: Exploration Geophysics, 34, 56-50.
  19. Reid, J. E., and Vrbancich, J., 2004, A comparison of the inductive-limit footprints of airborne electromagnetic systems: Geophysics (in press).
  20. Sattel, D., 1998, Conductivity information in three dimensions: Geophysics, 29, 157-162.
  21. Smith, B. D., Irvine, R., Blome, C, Clark, A., and Smith, D.V, 2003, Preliminary results, helicopter electromagnetic and magnetic survey of the Seco Creek area, Medina and Uvalde counties, Texas: Symposium on the Application of Geophysics to Engineering and Environmental Problems (SAGEEP) 2003, EEGS, 403-418.
  22. Smith, R. S., and Annan, A.P, 1997, Advances in airborne time-domain EM technology: in Gubins, A. G., (ed.), Proceedings of Exploration 97: Fourth Decennial International Conference on Mineral Exploration, 497-504.
  23. Stolz, KM. and Macnae, J., 1998, Evaluating EM waveforms by singular-value decomposition of exponential basis functions: Geophysics, 63, 64-74.
  24. Yin, C, and Fraser, D. C., 2003, Attitude corrections of helicopter EM data using a superposed dipole model: Geophysics, 69, 431-439.
/content/journals/10.1071/EG04208
Loading
  • Article Type: Research Article
Keyword(s): Airborne electromagnetics; EM modelling; GEOTEM; RESOLVE; TEMPEST

Most Cited This Month Most Cited RSS feed

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