2020
DOI: 10.1002/nsg.12134
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A numerical dispersion‐suppressed method for shallow seismic migration

Abstract: Reverse time migration can accurately image underground earth structures. However, for shallow seismic exploration, the seismic wave velocity is often lower than the velocity in the middle‐deep layers, which causes numerical dispersion for finite‐difference schemes and leads to poor seismic imaging quality. Suppressing numerical dispersion by grid encryption or increasing the finite‐difference order seriously reduces computational efficiency, which is not the optimal solution. To improve the imaging quality wi… Show more

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Cited by 2 publications
(1 citation statement)
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“…Accurate detection of the goaf is the premise of stability analysis and treatment of goaf. The main methods used in the area of cavity detection include the high-density resistivity method [6], seismic image method [7], ground-penetrating radar method [8], transient rayleigh wave method [9] and laser three-dimensional scanning method [10]. With the increasing complexity and number of goaf, the requirements of engineers for detection accuracy have gradually increased, and the results obtained by geophysical exploration means cannot have a substantial effect on the treatment of mined areas.…”
Section: Introductionmentioning
confidence: 99%
“…Accurate detection of the goaf is the premise of stability analysis and treatment of goaf. The main methods used in the area of cavity detection include the high-density resistivity method [6], seismic image method [7], ground-penetrating radar method [8], transient rayleigh wave method [9] and laser three-dimensional scanning method [10]. With the increasing complexity and number of goaf, the requirements of engineers for detection accuracy have gradually increased, and the results obtained by geophysical exploration means cannot have a substantial effect on the treatment of mined areas.…”
Section: Introductionmentioning
confidence: 99%