Forming an image of complex parts of the structure of the refracting boundary

Migration transformations of the field of refracted waves make possible imaging of structural features of irregularly shaped refraction boundary in deep dynamic section. First arrivals of refracted waves are persistently traced on the wave field along considerable distances from the source of wave e...

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Datum:2012
1. Verfasser: Verpahovskaya, A. O.
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/116671
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Geofizicheskiy Zhurnal
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author Verpahovskaya, A. O.
author_facet Verpahovskaya, A. O.
author_sort Verpahovskaya, A. O.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T12:21:20Z
description Migration transformations of the field of refracted waves make possible imaging of structural features of irregularly shaped refraction boundary in deep dynamic section. First arrivals of refracted waves are persistently traced on the wave field along considerable distances from the source of wave excitation that is a guarantee of a high definition of recreation of structural details of the studied boundary while processing the data of regional seismic exploration. Special features of accomplishment of finite-difference migration of the refracted wave field under conditions of refracting boundary structure complicated by faults have been considered as well as methodic problems, related to valuation of the wave field interval where refracted waves are registered depending on the velocity model of the medium. The results of the studies are demonstrated on the model and practical materials.
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spelling journalsuranua-geofizicheskiy-article-1166712020-10-07T12:21:20Z Forming an image of complex parts of the structure of the refracting boundary Verpahovskaya, A. O. Migration transformations of the field of refracted waves make possible imaging of structural features of irregularly shaped refraction boundary in deep dynamic section. First arrivals of refracted waves are persistently traced on the wave field along considerable distances from the source of wave excitation that is a guarantee of a high definition of recreation of structural details of the studied boundary while processing the data of regional seismic exploration. Special features of accomplishment of finite-difference migration of the refracted wave field under conditions of refracting boundary structure complicated by faults have been considered as well as methodic problems, related to valuation of the wave field interval where refracted waves are registered depending on the velocity model of the medium. The results of the studies are demonstrated on the model and practical materials. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2012-10-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116671 10.24028/gzh.0203-3100.v34i5.2012.116671 Geofizicheskiy Zhurnal; Vol. 34 No. 5 (2012); 150-160 Геофизический журнал; Том 34 № 5 (2012); 150-160 Геофізичний журнал; Том 34 № 5 (2012); 150-160 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/116671/110747 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle Verpahovskaya, A. O.
Forming an image of complex parts of the structure of the refracting boundary
title Forming an image of complex parts of the structure of the refracting boundary
title_full Forming an image of complex parts of the structure of the refracting boundary
title_fullStr Forming an image of complex parts of the structure of the refracting boundary
title_full_unstemmed Forming an image of complex parts of the structure of the refracting boundary
title_short Forming an image of complex parts of the structure of the refracting boundary
title_sort forming an image of complex parts of the structure of the refracting boundary
url https://journals.uran.ua/geofizicheskiy/article/view/116671
work_keys_str_mv AT verpahovskayaao forminganimageofcomplexpartsofthestructureoftherefractingboundary