Geometric 2.5D inversion of marine time domain electromagnetic data with application to hydrocarbon deposits prospecting

• Published in: Journal of applied geophysics 2023-05, Vol.212, p.104996, Article 104996
• Main Authors: Persova, Marina G., Soloveichik, Yuri G., Kjerstad, Jostein K., Sivenkova, Anastasia P., Kiseleva, Anna S., Kiselev, Dmitry S.
• Format: Article
• Language: English
• Subjects: Electromagnetic data interpretation; Marine electromagnetic prospecting; Marine hydrocarbon deposits
• ISSN: 0926-9851; 1879-1859
• DOI: 10.1016/j.jappgeo.2023.104996

To solve the problem of detection and delineation of marine hydrocarbon deposits located at different depths in an inhomogeneous medium, we propose an approach to 2.5D inversion of electromagnetic (EM) data measured in the time domain (TD) using a differentially normalized method of electrical prospecting. The approach is based on geometric inversion, in which block structures are used to parameterize the geological medium. The sizes of blocks in the initial model are set depending on the depth. Bathymetry is taken into account as a 3D surface. As a result of inversion, the coordinates of block boundaries and conductivity inside blocks and layers are determined. The minimized functional is represented as a sum of weighted residuals between computed and practical data and regularizing terms. Adaptive regularization is used to satisfy parameter constraints. To solve a 3D forward problem and calculate derivatives with respect to parameters, the finite element method (FEM) is used. We propose to use a priori data on the depth of the target layers and use various options of block structures with an analysis of possible uncertainties in detecting target bodies and determining their boundaries. We present the results of a 2.5D inversion of field data obtained in one of the areas in the North Sea. Target bodies discovered as a result of inversion are confirmed by well data. Coincidences were obtained both for productive wells and for dry ones. Using synthetic data for various geoelectric models and options of block structures, we justify the proposed approach to the inversion of marine TD EM data and make recommendations for its use. •The second potential difference allows marine HC deposits discovery in complex media.•Geometric 2.5D inversion allows delineating marine HC deposits with weak response.•The seafloor bathymetry should be considered as a 3D surface.•The inversion method is justified using synthetic data for various geoelectric models.•The results of field data inversion in the North Sea are confirmed by well data.