Please use this identifier to cite or link to this item: http://repositorio.unicamp.br/jspui/handle/REPOSIP/345359
Type: Artigo
Title: Limitations of correlation-based redatuming methods
Author: Barrera P., D. F.
Schleicher, J.
van der Neut, J.
Abstract: Redatuming aims to correct seismic data for the consequences of an acquisition far from the target. That includes the effects of an irregular acquisition surface and of complex geological structures in the overburden such as strong lateral heterogeneities or layers with low or very high velocity. Interferometric techniques can be used to relocate sources to positions where only receivers are available and have been used to move acquisition geometries to the ocean bottom or transform data between surface-seismic and vertical seismic profiles. Even if no receivers are available at the new datum, the acquisition system can be relocated to any datum in the subsurface to which the propagation of waves can be modeled with sufficient accuracy. By correlating the modeled wavefield with seismic surface data, one can carry the seismic acquisition geometry from the surface closer to geologic horizons of interest. Specifically, we show the derivation and approximation of the one-sided seismic interferometry equation for surface-data redatuming, conveniently using Green's theorem for the Helmholtz equation with density variation. Our numerical examples demonstrate that correlation-based single-boundary redatuming works perfectly in a homogeneous overburden. If the overburden is inhomogeneous, primary reflections from deeper interfaces are still repositioned with satisfactory accuracy. However, in this case artifacts are generated as a consequence of incorrectly redatumed overburden multiples. These artifacts get even worse if the complete wavefield is used instead of the direct wavefield. Therefore, we conclude that correlation-based interferometric redatuming of surface-seismic data should always be applied using direct waves only, which can be approximated with sufficient quality if a smooth velocity model for the overburden is available.
Subject: Prospecção sísmica
Interferometria
Ondas sísmicas
Geofísica - Modelos matemáticos
Interferometry
Seismic prospecting
Seismic waves
Geophysics – Mathematical models
Country: Reino Unido
Editor: Oxford University Press
Rights: aberto
Identifier DOI: 10.1088/1742-2140/aa83cb
Address: https://iopscience.iop.org/article/10.1088/1742-2140/aa83cb/meta
Date Issue: 2017
Appears in Collections:IMECC - Artigos e Outros Documentos
FEM - Artigos e Outros Documentos

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