2016
DOI: 10.1190/geo2015-0513.1
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A hybrid finite-difference and integral-equation method for modeling and inversion of marine controlled-source electromagnetic data

Abstract: One of the major problems in the modeling and inversion of marine controlled-source electromagnetic (CSEM) data is related to the need for accurate representation of very complex geoelectrical models typical for marine environment. At the same time, the corresponding forward-modeling algorithms should be powerful and fast enough to be suitable for repeated use in hundreds of iterations of the inversion and for multiple transmitter/receiver positions. To this end, we have developed a novel 3D modeling and inver… Show more

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Cited by 45 publications
(5 citation statements)
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“…The 3D modeling and sensitivity calculations are based on the hybrid finite difference (FD) and integral equation (IE) method [29,30]. This technique employs an anomalous field formulation where the total field is split into background and anomalous fields,…”
Section: Three-dimensional Modeling and Inversion Using Hybrid Finite...mentioning
confidence: 99%
“…The 3D modeling and sensitivity calculations are based on the hybrid finite difference (FD) and integral equation (IE) method [29,30]. This technique employs an anomalous field formulation where the total field is split into background and anomalous fields,…”
Section: Three-dimensional Modeling and Inversion Using Hybrid Finite...mentioning
confidence: 99%
“…In the presented scheme, forward modelling is employed only for the generation of synthetic data used in NN training. For the spatial discretization of Equation (3), I use the 3-D finite-difference method based on staggered grids that is still commonly applied in geophysical problems (e.g., Kelbert et al, 2014;Jaysaval et al, 2014;Commer et al, 2015;Yoon et al, 2016). The details of the forward modelling algorithm are given in Appendix A.…”
Section: Problem Formulation 21 Forward Modellingmentioning
confidence: 99%
“…For a loop source, we only need to assign values to the source vectors of J x and J y , as J z is always a zero vector. According to equation 5, we substitute equations (6) to (8) into equations (9) to (11); then, we can obtain equations (12) to (14), as shown at the bottom of the next page. According to Ax = b, the components in equations (12) to 14can be expressed as equations (15) to (17), as shown at the bottom of the next page.…”
Section: A Three-dimensional Fdfd Numerical Simulation Theorymentioning
confidence: 99%
“…Then, he analyzed the influence of grid spacing on the calculation error and deduced the corresponding error expression. Yoon [14] combined FDFD with the integral equation method for numerical simulation of marine controllable sources. First, the electric field component is calculated by the FDFD method, and then the magnetic field at the receiver is calculated accurately by the integral equation method to reduce the computational complexity.…”
Section: Introductionmentioning
confidence: 99%