Depth to magnetic source estimation using TDX contour

TL;DR

This paper introduces a rapid and noise-resistant method for estimating the depth of magnetic sources using the TDX derivative of the magnetic field, improving accuracy in geophysical applications.

Contribution

It presents a novel approach utilizing the TDX contour for depth estimation, demonstrating effectiveness with models and assumptions suitable for practical geophysical scenarios.

Findings

Method accurately estimates source depth in models

Effective even with noisy magnetic data

Reliable for sources with complex fault structures

Abstract

Accurate depth estimation of magnetic sources plays a crucial role in various geophysical applications, including mineral exploration, resource assessments, regional hydrocarbon exploration, and geological mapping. Thus, this abstract presents a fast and simple method of estimating the depth of a magnetic body using the TDX derivative of the total magnetic field. TDX is a first-order derivative of the magnetic field that, in addition to edge detection, is less affected by noise, allowing for better depth resolution. The reduced sensitivity to noise enables a clearer estimation of depth and enhances the accuracy of the depth determination process. The TDX, as a variant of the phase derivative, is independent of magnetization and can be used to identify the edge of a magnetic body. In addition to excelling at edge detection, they can also estimate the depth of the magnetic source producing the anomalies. In this study, we explore the utilization of contour of the TDX derivative for estimating depth, assuming a vertical contact source. We demonstrate the effectiveness of the method using a two-prism block model and a simple bishop model with a uniform susceptibility of 0.001 cgs. The results agree with the known depth, providing evidence of the reliability of the method despite the restrictive nature of the assumption, especially for the Bishop model, where there are numerous fault structures.