1887

Abstract

Summary

Conductivity-depth imaging is a common method for the interpretation of airborne transient electromagnetic data. The interpretation of Semi-airborne transient electromagnetic data is similar to the airborne transient electromagnetic method, due to the large amount of data, the similar imaging method is also required. In this paper we present a SATEM CDI method which based on nonlinear implicit function, and use one field data to verify the practicability of this method, and we also compared the CDI results with the geological information and ground inversion results. The results demonstrate that this CDI method is practical for SATEM data.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201800390
2018-04-09
2024-04-23
Loading full text...

Full text loading...

References

  1. MogiT., KusunokiK., KaiedaH., et al.
    2009. Grounded electrical-source airborne transient electromagnetic (GREATEM) survey of Mount Bandai, north-eastern Japan. Exploration Geophysics, 40, 1–7.
    [Google Scholar]
  2. MacnaeJ. C., SmithR., PolzerB. D., et al.
    1991. Conductivity-depth imaging of airborne electromagnetic step-response data. Geophysics, 56, 102–114.
    [Google Scholar]
  3. HuangH. P., RuddJ.
    2008. Conductivity-depth imaging of helicopter-borne TEM data based on a pseudolayer half-space model. Geophysics, 73, 115–120.
    [Google Scholar]
  4. MaoL. F.
    2013. Conductivity-depth imaging algorithm for central-loop helicopter TEM. CT Theory and Applications (in Chinese), 22, 429–437.
    [Google Scholar]
http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201800390
Loading
/content/papers/10.3997/2214-4609.201800390
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