A Two-Dimensional Amplitude Study of True-Amplitude Time Migration and Time Remigration – 2.5-D Synthetic Examples

In this synthetic study, we present semi-automatically picked true-amplitude comparisons after time migration and time remigration (Tygel et al.,1996; and Oliveira et al.,2023). Since the examples considered are synthetic, emphasis is put on the generally disregarded dimensional aspects of the amplitudes that are modeled to simulate compressional-only seismic data when using a Kirchhoff a p proximation. By bearing in mind in this work that theoretical amplitudes work as “densities”, we show that when comparisons of true-amplitude weighted diffraction-stack time migration and weighted isochrone-stack time remigration are performed, in order to “correct” the dimensions involved certain multiplicative physical constants must come into play and that must be effectively dealt with, for plotting reasons.

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Publication Details

Journal
Brazilian Journal of Geophysics
Published
2024-09-12
DOI
https://doi.org/10.22564/brjg.v42i2.2319
Primary Topic
Machine Fault Diagnosis Techniques
Type
article
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article

A Two-Dimensional Amplitude Study of True-Amplitude Time Migration and Time Remigration – 2.5-D Synthetic Examples

Karina Palheta Gomes, A. S. A. Oliveira, Carlos Augusto Sarmento Ferreira
Brazilian Journal of Geophysics
Machine Fault Diagnosis Techniques
article

A Two-Dimensional Amplitude Study of True-Amplitude Time Migration and Time Remigration – 2.5-D Synthetic Examples

Karina Palheta Gomes, A. S. A. Oliveira, Carlos Augusto Sarmento Ferreira
article en

Abstract

In this synthetic study, we present semi-automatically picked true-amplitude comparisons after time migration and time remigration (Tygel et al.,1996; and Oliveira et al.,2023). Since the examples considered are synthetic, emphasis is put on the generally disregarded dimensional aspects of the amplitudes that are modeled to simulate compressional-only seismic data when using a Kirchhoff a p proximation. By bearing in mind in this work that theoretical amplitudes work as “densities”, we show that when comparisons of true-amplitude weighted diffraction-stack time migration and weighted isochrone-stack time remigration are performed, in order to “correct” the dimensions involved certain multiplicative physical constants must come into play and that must be effectively dealt with, for plotting reasons.

Brazilian Journal of GeophysicsVol. 42(2)
Universidade Federal do Acre (BR), Valongo Observatory (BR), National Observatory (BR)
Openalex Percentile: Top 78%
Machine Fault Diagnosis Techniques
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