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Detection of a waveguide in the basement of the northwestern shelf of the Black Sea according to the results of reinterpretation of the DSS materials of profiles 26 and 25

Results of reinterpretation of DSS materials along the profiles worked out within north-western shelf of the Black Sea near 45 years ago are given. Those are two seismic profiles crossed the shelf area: latitudinal DSS Profile 26 (Zmiyinyi Island - Tarkhankut Peninsula) and Profile 25, which crosses...

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Main Authors: Baranova, E. P., Egorova, T.P., Omelchenko, V. D.
Format: Article
Language:rus
Published: Subbotin Institute of Geophysics of the NAS of Ukraine 2011
Online Access:https://journals.uran.ua/geofizicheskiy/article/view/116790
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spelling journalsuranua-geofizicheskiy-article-1167902020-10-07T11:02:57Z Detection of a waveguide in the basement of the northwestern shelf of the Black Sea according to the results of reinterpretation of the DSS materials of profiles 26 and 25 Baranova, E. P. Egorova, T.P. Omelchenko, V. D. Results of reinterpretation of DSS materials along the profiles worked out within north-western shelf of the Black Sea near 45 years ago are given. Those are two seismic profiles crossed the shelf area: latitudinal DSS Profile 26 (Zmiyinyi Island - Tarkhankut Peninsula) and Profile 25, which crosses the western part of the Black Sea in sub-longitudinal direction. The wave field is character-ised by some special features in observed travel-time curves, which are indicative on the presence of wave guides here (the layers with decreased velocities). Velocity simulation produced by ray-tracing method along two profiles 26 and 25 indicated the presence in the basement and the upper part of consolidated crust of an inversion zone of complicated structure.The nature of a distinguished zone might by related to the occurrence of fault zones filled with rocks of increased jointing and porosity and the fluids, which may have under conditions of the north-western shelf hydrocarbon composition. Subbotin Institute of Geophysics of the NAS of Ukraine 2011-12-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116790 10.24028/gzh.0203-3100.v33i6.2011.116790 Geofizicheskiy Zhurnal; Vol. 33 No. 6 (2011); 15-29 Геофизический журнал; Том 33 № 6 (2011); 15-29 Геофізичний журнал; Том 33 № 6 (2011); 15-29 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/116790/110850 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
collection OJS
language rus
format Article
author Baranova, E. P.
Egorova, T.P.
Omelchenko, V. D.
spellingShingle Baranova, E. P.
Egorova, T.P.
Omelchenko, V. D.
Detection of a waveguide in the basement of the northwestern shelf of the Black Sea according to the results of reinterpretation of the DSS materials of profiles 26 and 25
author_facet Baranova, E. P.
Egorova, T.P.
Omelchenko, V. D.
author_sort Baranova, E. P.
title Detection of a waveguide in the basement of the northwestern shelf of the Black Sea according to the results of reinterpretation of the DSS materials of profiles 26 and 25
title_short Detection of a waveguide in the basement of the northwestern shelf of the Black Sea according to the results of reinterpretation of the DSS materials of profiles 26 and 25
title_full Detection of a waveguide in the basement of the northwestern shelf of the Black Sea according to the results of reinterpretation of the DSS materials of profiles 26 and 25
title_fullStr Detection of a waveguide in the basement of the northwestern shelf of the Black Sea according to the results of reinterpretation of the DSS materials of profiles 26 and 25
title_full_unstemmed Detection of a waveguide in the basement of the northwestern shelf of the Black Sea according to the results of reinterpretation of the DSS materials of profiles 26 and 25
title_sort detection of a waveguide in the basement of the northwestern shelf of the black sea according to the results of reinterpretation of the dss materials of profiles 26 and 25
description Results of reinterpretation of DSS materials along the profiles worked out within north-western shelf of the Black Sea near 45 years ago are given. Those are two seismic profiles crossed the shelf area: latitudinal DSS Profile 26 (Zmiyinyi Island - Tarkhankut Peninsula) and Profile 25, which crosses the western part of the Black Sea in sub-longitudinal direction. The wave field is character-ised by some special features in observed travel-time curves, which are indicative on the presence of wave guides here (the layers with decreased velocities). Velocity simulation produced by ray-tracing method along two profiles 26 and 25 indicated the presence in the basement and the upper part of consolidated crust of an inversion zone of complicated structure.The nature of a distinguished zone might by related to the occurrence of fault zones filled with rocks of increased jointing and porosity and the fluids, which may have under conditions of the north-western shelf hydrocarbon composition.
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2011
url https://journals.uran.ua/geofizicheskiy/article/view/116790
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AT egorovatp detectionofawaveguideinthebasementofthenorthwesternshelfoftheblackseaaccordingtotheresultsofreinterpretationofthedssmaterialsofprofiles26and25
AT omelchenkovd detectionofawaveguideinthebasementofthenorthwesternshelfoftheblackseaaccordingtotheresultsofreinterpretationofthedssmaterialsofprofiles26and25
first_indexed 2024-04-21T19:41:23Z
last_indexed 2024-04-21T19:41:23Z
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