Finite-difference wave migration of initial seismograms of a common point of explosion in the time domain

The final procedure of the standard production processing and interpretation of seismic data is the post-stack migration by the central deep point method (CDP). However, in practice, a more informative image of the deep section is given by the pre-stack migration according to initial seismograms. Th...

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Datum:2012
Hauptverfasser: Pilipenko, V.N., Verpakhovskaya, A. O., Gnevush, V. V.
Format: Artikel
Sprache:Russisch
Veröffentlicht: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2012
Online Zugang:https://journals.uran.ua/geofizicheskiy/article/view/116636
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Geofizicheskiy Zhurnal
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author Pilipenko, V.N.
Verpakhovskaya, A. O.
Gnevush, V. V.
author_facet Pilipenko, V.N.
Verpakhovskaya, A. O.
Gnevush, V. V.
author_sort Pilipenko, V.N.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T12:21:30Z
description The final procedure of the standard production processing and interpretation of seismic data is the post-stack migration by the central deep point method (CDP). However, in practice, a more informative image of the deep section is given by the pre-stack migration according to initial seismograms. The actual task of processing and interpretation of the observed wave field to produce the image of the deep structure without the procedure of the CDP stack is presented. This solution is implemented using a new version of the finite-difference pre-stack migration of the shot record in time domain. The advantages and possibilities of applications of this method are shown in model and real examples.
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spelling journalsuranua-geofizicheskiy-article-1166362020-10-07T12:21:30Z Finite-difference wave migration of initial seismograms of a common point of explosion in the time domain Pilipenko, V.N. Verpakhovskaya, A. O. Gnevush, V. V. The final procedure of the standard production processing and interpretation of seismic data is the post-stack migration by the central deep point method (CDP). However, in practice, a more informative image of the deep section is given by the pre-stack migration according to initial seismograms. The actual task of processing and interpretation of the observed wave field to produce the image of the deep structure without the procedure of the CDP stack is presented. This solution is implemented using a new version of the finite-difference pre-stack migration of the shot record in time domain. The advantages and possibilities of applications of this method are shown in model and real examples. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2012-06-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116636 10.24028/gzh.0203-3100.v34i3.2012.116636 Geofizicheskiy Zhurnal; Vol. 34 No. 3 (2012); 40-48 Геофизический журнал; Том 34 № 3 (2012); 40-48 Геофізичний журнал; Том 34 № 3 (2012); 40-48 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/116636/110674 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle Pilipenko, V.N.
Verpakhovskaya, A. O.
Gnevush, V. V.
Finite-difference wave migration of initial seismograms of a common point of explosion in the time domain
title Finite-difference wave migration of initial seismograms of a common point of explosion in the time domain
title_full Finite-difference wave migration of initial seismograms of a common point of explosion in the time domain
title_fullStr Finite-difference wave migration of initial seismograms of a common point of explosion in the time domain
title_full_unstemmed Finite-difference wave migration of initial seismograms of a common point of explosion in the time domain
title_short Finite-difference wave migration of initial seismograms of a common point of explosion in the time domain
title_sort finite-difference wave migration of initial seismograms of a common point of explosion in the time domain
url https://journals.uran.ua/geofizicheskiy/article/view/116636
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AT gnevushvv finitedifferencewavemigrationofinitialseismogramsofacommonpointofexplosioninthetimedomain