Title of article
Depth Estimates for Slingram Electromagnetic Anomalies from Dipping Sheet-like Bodies by the Normalized Full Gradient Method
Author/Authors
Derman Dondurur، نويسنده ,
Issue Information
ماهنامه با شماره پیاپی سال 2005
Pages
17
From page
2179
To page
2195
Abstract
The Normalized Full Gradient (NFG) method was proposed in the mid–1960s and was
generally used for the downward continuation of the potential field data. The method eliminates the side
oscillations which appeared on the continuation curves when passing through anomalous body depth. In
this study, the NFG method was applied to Slingram electromagnetic anomalies to obtain the depth of the
anomalous body. Some experiments were performed on the theoretical Slingram model anomalies in a free
space environment using a perfectly conductive thin tabular conductor with an infinite depth extent. The
theoretical Slingram responses were obtained for different depths, dip angles and coil separations, and it
was observed from NFG fields of the theoretical anomalies that the NFG sections yield the depth
information of top of the conductor at low harmonic numbers. The NFG sections consisted of two main
local maxima located at both sides of the central negative Slingram anomalies. It is concluded that these
two maxima also locate the maximum anomaly gradient points, which indicates the depth of the anomaly
target directly. For both theoretical and field data, the depth of the maximum value on the NFG sections
corresponds to the depth of the upper edge of the anomalous conductor. The NFG method was applied to
the in-phase component and correct depth estimates were obtained even for the horizontal tabular
conductor. Depth values could be estimated with a relatively small error percentage when the conductive
model was near-vertical and/or the conductor depth was larger.
Keywords
Slingram anomalies , depthestimates. , downward continuation , Normalized Full Gradient Method
Journal title
Pure and Applied Geophysics
Serial Year
2005
Journal title
Pure and Applied Geophysics
Record number
429887
Link To Document