1887

Abstract

Euler deconvolution is routinely used in the interpretation of aeromagnetic data, but the method<br>has a tendency to produce vast numbers of solutions, all corresponding to slightly different<br>geological geometries. Wavelet transforms can be used to give information on the scales and<br>locations of features in the data, and this information can be used to determine improved<br>parameters for the Euler deconvolution. This results in output that is easier to interpret and which<br>reflects the true geology more accurately.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609-pdb.221.066
1999-09-28
2024-04-19
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.221.066
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