Features of processing of marine seismic observations using finite-difference full-wave migration

Features and basic principles of plotting the graph of marine seismic observations processing with application of original method of finite-difference total wave migration of the sum of central middle point, which is more stabile in case of investigation of complicated geological sections have been...

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Datum:2013
Hauptverfasser: Verpahovskaya, A. O., Pilipenko, V. N., Kobolev, V. P.
Format: Artikel
Sprache:Russisch
Veröffentlicht: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2013
Online Zugang:https://journals.uran.ua/geofizicheskiy/article/view/116447
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Назва журналу:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
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author Verpahovskaya, A. O.
Pilipenko, V. N.
Kobolev, V. P.
author_facet Verpahovskaya, A. O.
Pilipenko, V. N.
Kobolev, V. P.
author_sort Verpahovskaya, A. O.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T11:59:47Z
description Features and basic principles of plotting the graph of marine seismic observations processing with application of original method of finite-difference total wave migration of the sum of central middle point, which is more stabile in case of investigation of complicated geological sections have been considered. The effectiveness of the method is demonstrated on materials of seismic marine observations performed on the continental slope of northwestern shelf of the Black Sea.
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spelling journalsuranua-geofizicheskiy-article-1164472020-10-07T11:59:47Z Features of processing of marine seismic observations using finite-difference full-wave migration Verpahovskaya, A. O. Pilipenko, V. N. Kobolev, V. P. Features and basic principles of plotting the graph of marine seismic observations processing with application of original method of finite-difference total wave migration of the sum of central middle point, which is more stabile in case of investigation of complicated geological sections have been considered. The effectiveness of the method is demonstrated on materials of seismic marine observations performed on the continental slope of northwestern shelf of the Black Sea. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2013-10-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116447 10.24028/gzh.0203-3100.v35i5.2013.116447 Geofizicheskiy Zhurnal; Vol. 35 No. 5 (2013); 187-195 Геофизический журнал; Том 35 № 5 (2013); 187-195 Геофізичний журнал; Том 35 № 5 (2013); 187-195 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/116447/110477 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle Verpahovskaya, A. O.
Pilipenko, V. N.
Kobolev, V. P.
Features of processing of marine seismic observations using finite-difference full-wave migration
title Features of processing of marine seismic observations using finite-difference full-wave migration
title_full Features of processing of marine seismic observations using finite-difference full-wave migration
title_fullStr Features of processing of marine seismic observations using finite-difference full-wave migration
title_full_unstemmed Features of processing of marine seismic observations using finite-difference full-wave migration
title_short Features of processing of marine seismic observations using finite-difference full-wave migration
title_sort features of processing of marine seismic observations using finite-difference full-wave migration
url https://journals.uran.ua/geofizicheskiy/article/view/116447
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AT pilipenkovn featuresofprocessingofmarineseismicobservationsusingfinitedifferencefullwavemigration
AT kobolevvp featuresofprocessingofmarineseismicobservationsusingfinitedifferencefullwavemigration