Abstract
Three depth migration methods which operate on common-shot data are presented. The first migration method maps digitized horizons from the X-T domain to the X-Z domain. Because this method is based on ray tracing, its computation time is short; it is suggested for iterative velocity analysis. The other 2 migration methods map the entire common-shot gather into a depth section. The common-shot migration requires calculation of the arrival time of the direct wave from the source to all the depth points, and is done through a direct solution of the eikonal equation. All 3 methods are suitable for areas with both lateral and vertical velocity variation.- Authors
Original language | English |
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Pages (from-to) | 324-331 |
Number of pages | 8 |
Journal | Geophysics |
Volume | 51 |
Issue number | 2 |
DOIs | |
State | Published - 1986 |