Generalized magnetic tilt-Euler deconvolution

Ahmed Salem; Richard Smith; Simon Williams; Dhananjay Ravat; Derek Fairhead

doi:10.1190/1.2792530

Generalized magnetic tilt-Euler deconvolution

Ahmed Salem, Richard Smith, Simon Williams, Dhananjay Ravat, Derek Fairhead

Research output: Contribution to journal › Article › peer-review

3 Scopus citations

Abstract

We introduce Euler deconvolution of the magnetic tilt angle. The magnetic tilt angle is a generalized definition of the local phase. In the Generalized Tilt-Euler deconvolution method, no structural index is required. As a result the method can provide automatic estimates of source location from gridded magnetic data using second order derivatives. The method is tested using theoretical data for simple and complicated magnetic models and provided good results.

Original language	English
Pages (from-to)	790-794
Number of pages	5
Journal	SEG Technical Program Expanded Abstracts
Volume	26
Issue number	1
DOIs	https://doi.org/10.1190/1.2792530
State	Published - Jan 2007

ASJC Scopus subject areas

Geotechnical Engineering and Engineering Geology
Geophysics

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title = "Generalized magnetic tilt-Euler deconvolution",

abstract = "We introduce Euler deconvolution of the magnetic tilt angle. The magnetic tilt angle is a generalized definition of the local phase. In the Generalized Tilt-Euler deconvolution method, no structural index is required. As a result the method can provide automatic estimates of source location from gridded magnetic data using second order derivatives. The method is tested using theoretical data for simple and complicated magnetic models and provided good results.",

author = "Ahmed Salem and Richard Smith and Simon Williams and Dhananjay Ravat and Derek Fairhead",

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AU - Williams, Simon

AU - Ravat, Dhananjay

AU - Fairhead, Derek

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AB - We introduce Euler deconvolution of the magnetic tilt angle. The magnetic tilt angle is a generalized definition of the local phase. In the Generalized Tilt-Euler deconvolution method, no structural index is required. As a result the method can provide automatic estimates of source location from gridded magnetic data using second order derivatives. The method is tested using theoretical data for simple and complicated magnetic models and provided good results.

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Generalized magnetic tilt-Euler deconvolution

Abstract

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