Formation geological depth image according to refraction and reflection marine seismic data

The possibility of forming of the geological depth image from marine seismic data observed with the method of reflected waves by multiple overlaps and the refracted method by deep seismic sounding was investigated. The difference in the algorithms for the creating of depth image using the finite-dif...

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Бібліографічні деталі
Дата:2017
Автори: Verpahovskaya, A. O., Pilipenko, V. N., Pylypenko, Е. V.
Формат: Стаття
Мова:rus
Опубліковано: Subbotin Institute of Geophysics of the NAS of Ukraine 2017
Теми:
Онлайн доступ:https://journals.uran.ua/geofizicheskiy/article/view/116375
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Назва журналу:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
id journalsuranua-geofizicheskiy-article-116375
record_format ojs
spelling journalsuranua-geofizicheskiy-article-1163752020-10-07T11:16:57Z Formation geological depth image according to refraction and reflection marine seismic data Verpahovskaya, A. O. Pilipenko, V. N. Pylypenko, Е. V. reflected refracted wave methods deep seismic sounding formation of a deep image finite-difference migration continuation of the wave and time fields refracted waves The possibility of forming of the geological depth image from marine seismic data observed with the method of reflected waves by multiple overlaps and the refracted method by deep seismic sounding was investigated. The difference in the algorithms for the creating of depth image using the finite-difference migration on the field of reflected and refracted waves is shown. Also there is presented the possibility of comparing and generalizing their results. Researches were carried out using the example of seismic data, observed with the method of reflected waves by multiple overlaps and the refracted method by deep seismic sounding in the area of the Azov Sea. Subbotin Institute of Geophysics of the NAS of Ukraine 2017-11-30 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116375 10.24028/gzh.0203-3100.v39i6.2017.116375 Geofizicheskiy Zhurnal; Vol. 39 No. 6 (2017); 106-121 Геофизический журнал; Том 39 № 6 (2017); 106-121 Геофізичний журнал; Том 39 № 6 (2017); 106-121 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/116375/111008 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
collection OJS
language rus
topic reflected
refracted wave methods
deep seismic sounding
formation of a deep image
finite-difference migration
continuation of the wave and time fields
refracted waves
spellingShingle reflected
refracted wave methods
deep seismic sounding
formation of a deep image
finite-difference migration
continuation of the wave and time fields
refracted waves
Verpahovskaya, A. O.
Pilipenko, V. N.
Pylypenko, Е. V.
Formation geological depth image according to refraction and reflection marine seismic data
topic_facet reflected
refracted wave methods
deep seismic sounding
formation of a deep image
finite-difference migration
continuation of the wave and time fields
refracted waves
format Article
author Verpahovskaya, A. O.
Pilipenko, V. N.
Pylypenko, Е. V.
author_facet Verpahovskaya, A. O.
Pilipenko, V. N.
Pylypenko, Е. V.
author_sort Verpahovskaya, A. O.
title Formation geological depth image according to refraction and reflection marine seismic data
title_short Formation geological depth image according to refraction and reflection marine seismic data
title_full Formation geological depth image according to refraction and reflection marine seismic data
title_fullStr Formation geological depth image according to refraction and reflection marine seismic data
title_full_unstemmed Formation geological depth image according to refraction and reflection marine seismic data
title_sort formation geological depth image according to refraction and reflection marine seismic data
description The possibility of forming of the geological depth image from marine seismic data observed with the method of reflected waves by multiple overlaps and the refracted method by deep seismic sounding was investigated. The difference in the algorithms for the creating of depth image using the finite-difference migration on the field of reflected and refracted waves is shown. Also there is presented the possibility of comparing and generalizing their results. Researches were carried out using the example of seismic data, observed with the method of reflected waves by multiple overlaps and the refracted method by deep seismic sounding in the area of the Azov Sea.
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2017
url https://journals.uran.ua/geofizicheskiy/article/view/116375
work_keys_str_mv AT verpahovskayaao formationgeologicaldepthimageaccordingtorefractionandreflectionmarineseismicdata
AT pilipenkovn formationgeologicaldepthimageaccordingtorefractionandreflectionmarineseismicdata
AT pylypenkoev formationgeologicaldepthimageaccordingtorefractionandreflectionmarineseismicdata
first_indexed 2024-04-21T19:40:45Z
last_indexed 2024-04-21T19:40:45Z
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