To effectively and efficiently interpret or invert controlled-source electromagnetic (CSEM)
data which are recorded in areas with the kind of complex geological environments and …

Unstructured grids are capable of faithfully representing real-life geologic models and
topography with relatively few mesh cells. We have developed a finite-volume solution to the …

We investigate an emerging method called surface geometry inversion (SGI) for the
inversion of transient electromagnetic (TEM) data. Conventional minimum-structure …

Numerical modeling of electromagnetic (EM) fields in a conductive marine environment is
crucial for marine EM data interpretation. During marine controlled-source electromagnetic …

Transient electromagnetic (TEM) modeling is a challenge in terms of memory and computing
time. TEM responses are affected by the full transmitting-current waveforms and needs to be …

The 3-D time-domain electromagnetic (TEM) modeling is computationally expensive. Shift-
and-invert (SAI) Krylov subspace technique has proved efficient for the modeling of OFF …

Controlled-source electromagnetic (CSEM) method is crucial for detecting and locating
underground anomalies and structures. However, it is challenging to interpret the field data …

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 …

The transient electromagnetic (TEM) method is a valuable tool for detecting the structure of
underground geological targets. However, TEM survey environments are complex and …

Krylov subspace projection model order reduction technique for matrix function has proved
efficient for the modeling of 3-D OFF-time transient electromagnetic (TEM) data. However …