Examples of Seismic Shallow Subsurface Characterisation and Deep Electromagnetic Monitoring

Difficulties in detecting and characterising shallow objects close the surface with seismic shear waves are often problematic because of dominant surface waves. By sequencing a specific combination of two data driven processing steps followed by diffraction tomography can overcome these problems. Small scattering objects become visible in the...

Time-Domain CSEM Modelling Using Frequency- and Laplace-Domain Computations

Modelling time-domain electromagnetic data with a frequency-domain code requires the computation of many<br/>frequencies for the Fourier transform. This can make it computationally very expensive when compared with timedomain codes. However, it has been shown that frequency-domain codes can be competitive if frequencydependent modelling grids...