Abstract
Two seismic modelling approaches, that is, two-dimensional pre-stack elastic finite-difference and one-dimensional convolution methods, are compared in a modelling exercise over the fluid-flow simulation model of a producing deep-water turbidite sandstone reservoir in the West of Shetland Basin. If the appropriate parameterization for one-dimensional convolution is used, the differences in three-dimensional and four-dimensional seismic responses from the two methods are negligible. The key parameters to ensure an accurate seismic response are a representative wavelet, the distribution of common-depth points and their associated angles of incidence. Conventional seismic images generated by the one-dimensional convolutional model suffer from lack of continuity because it only accounts for vertical resolution. After application of a lateral resolution function, the convolutional and finite-difference seismic images are very similar. Although transmission effects, internal multiples and P-to-S conversions are not included in our convolutional modelling, the subtle differences between images from the two methods indicates that such effects are of secondary nature in our study. A quantitative comparison of the (normalized root-mean-square) amplitude attributes and waveform kinematics indicates that the finite-difference approach does not offer any tangible benefit in our target-oriented seismic modelling case study, and the potential errors from one-dimensional convolution modelling are comparatively much smaller than the production-induced time-lapse changes.
Original language | English |
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Pages (from-to) | 1540-1553 |
Number of pages | 14 |
Journal | Geophysical Prospecting |
Volume | 68 |
Issue number | 5 |
Early online date | 24 Jan 2020 |
DOIs | |
Publication status | Published - Jun 2020 |
Keywords
- 1D convolution
- Finite-difference modelling
- Simulator-to-seismic modelling
- Time-lapse monitoring
ASJC Scopus subject areas
- Geophysics
- Geochemistry and Petrology