Application of Post-stack migration to seismicdata associated with fault structures

In hydrocarbon exploration, wave-equation migrationtechniques play an important role in imaging thecomplex geological structures. Usually, post-stack migrationscheme is applied to the seismic data to improve theresolution with restoration of dipping reflectors to theirtrue position. As a result, the...

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Main Authors: Koduru Anitha, Mohanty P. R
Format: Article
Language:English
Published: De Gruyter 2015-06-01
Series:Open Geosciences
Subjects:
Online Access:https://doi.org/10.1515/geo-2015-0009
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spelling doaj-0394e2701be1408392187c69784cd4652021-09-05T20:50:46ZengDe GruyterOpen Geosciences2391-54472015-06-017110.1515/geo-2015-0009geo-2015-0009Application of Post-stack migration to seismicdata associated with fault structuresKoduru Anitha0Mohanty P. R1Department of Applied Geophysics, Indian School ofMines, Dhanbad -826004Department of Applied Geophysics, Indian School ofMines, Dhanbad -826004In hydrocarbon exploration, wave-equation migrationtechniques play an important role in imaging thecomplex geological structures. Usually, post-stack migrationscheme is applied to the seismic data to improve theresolution with restoration of dipping reflectors to theirtrue position. As a result, the migrated time sections areinterpretable in terms of subsurface features. As a numericalstudy, three fault models are considered for the presentstudy. First of all, synthetic time sections are generatedcorresponding to three models. Later, post stack migrationschemes such as Gazdag(PS), Phase-shift with turningrays and reverse time migration (T-K) domain techniquesare applied in order to judge the imaging accuracy, preservationof true amplitude and computational speed. All thethree post stack time migrated sections delineate the structurewith their throw.However, the reverse time migrations(T-K) clearly delineate the reflectors in restoring the throwproperly with minimum computational time. In order totest the validity the numerical results, similar exercise hasbeen undertaken using field seismic data of KG basin, India.The results indicates that the field migrated sectionsare imaged. But, the reverse time migration (T-K ) providesthe best subsurface image with restoration of reflectorsand collapse of diffracted events with least computationaltime. Gazdag (PS) and Phase-Shift with turning migratedsection shows the reduction of amplitude whereas, the reversetime migration preserved the amplitude fully.https://doi.org/10.1515/geo-2015-0009gazdag migration (ps) phase-shift with turningrays migration reverse time migration (t-k) domain
collection DOAJ
language English
format Article
sources DOAJ
author Koduru Anitha
Mohanty P. R
spellingShingle Koduru Anitha
Mohanty P. R
Application of Post-stack migration to seismicdata associated with fault structures
Open Geosciences
gazdag migration (ps)
phase-shift with turningrays migration
reverse time migration (t-k) domain
author_facet Koduru Anitha
Mohanty P. R
author_sort Koduru Anitha
title Application of Post-stack migration to seismicdata associated with fault structures
title_short Application of Post-stack migration to seismicdata associated with fault structures
title_full Application of Post-stack migration to seismicdata associated with fault structures
title_fullStr Application of Post-stack migration to seismicdata associated with fault structures
title_full_unstemmed Application of Post-stack migration to seismicdata associated with fault structures
title_sort application of post-stack migration to seismicdata associated with fault structures
publisher De Gruyter
series Open Geosciences
issn 2391-5447
publishDate 2015-06-01
description In hydrocarbon exploration, wave-equation migrationtechniques play an important role in imaging thecomplex geological structures. Usually, post-stack migrationscheme is applied to the seismic data to improve theresolution with restoration of dipping reflectors to theirtrue position. As a result, the migrated time sections areinterpretable in terms of subsurface features. As a numericalstudy, three fault models are considered for the presentstudy. First of all, synthetic time sections are generatedcorresponding to three models. Later, post stack migrationschemes such as Gazdag(PS), Phase-shift with turningrays and reverse time migration (T-K) domain techniquesare applied in order to judge the imaging accuracy, preservationof true amplitude and computational speed. All thethree post stack time migrated sections delineate the structurewith their throw.However, the reverse time migrations(T-K) clearly delineate the reflectors in restoring the throwproperly with minimum computational time. In order totest the validity the numerical results, similar exercise hasbeen undertaken using field seismic data of KG basin, India.The results indicates that the field migrated sectionsare imaged. But, the reverse time migration (T-K ) providesthe best subsurface image with restoration of reflectorsand collapse of diffracted events with least computationaltime. Gazdag (PS) and Phase-Shift with turning migratedsection shows the reduction of amplitude whereas, the reversetime migration preserved the amplitude fully.
topic gazdag migration (ps)
phase-shift with turningrays migration
reverse time migration (t-k) domain
url https://doi.org/10.1515/geo-2015-0009
work_keys_str_mv AT koduruanitha applicationofpoststackmigrationtoseismicdataassociatedwithfaultstructures
AT mohantypr applicationofpoststackmigrationtoseismicdataassociatedwithfaultstructures
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