With geophysical surveys evolving from traditional 2D to 3D models, the large volume of
data adds challenges to inversion, especially when aiming to resolve complex 3D structures …

Abstract Effects of induced polarization (IP) can have an impact on time-domain
electromagnetic measurements (TEM) and may lead to sign reversals in the recorded …

The primary aim of my research is to improve the characterization of induced polarization
(IP) responses in airborne electromagnetic (AEM) survey data. The principal objectives are …

A Time Domain Electromagnetic (TDEM) survey was carried out in and around the caldera
of the Fogo volcano, Cape Verde Islands, to detect the low resistive structures that could be …

This paper seeks to explain the origin of sign reversal or zero-crossover effect observed at
late decay times in the experimental data involving the application of SQUID in geophysical …

The loop radius of the coincident-loop system above a polarizable half-space has a
significant effect on the magnitude of the negative response and its time of occurrence …

Recent advancements in the signal-to-noise ratio of transient electromagnetic (TEM) devices
have highlighted the significance of induced polarization (IP) effects in areas containing …

For several decades, induced polarization (IP) effects on transient electromagnetic (TEM)
responses have been observed. These effects can manifest as late-time negative transients …

In time domain electromagnetic central loop sounding or coincidence loop measurements
often a sign reversal is observed in the recorded decay transients. These negative decay …

The transient electromagnetic (TEM) method becomes more urgent than ever for marine
exploration due to abundant resource reserves and the increasing undersea engineering …