STRUCTURE MODELLING OF SUBSURFACE BY USING KIRCHHOFF MIGRATION METHOD AND FINITE DIFFERENCE ANISOTROPY METHOD
The image of subsurface with a migration method keeps on developing to get an image result which the closest in real condition. The conditions in subsurface are very complex and variables it couses the process of wave propagation which can not be judged as the same in every layers. so it is needed...
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Sebelas Maret University
2017-02-01
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Series: | Indonesian Journal of Applied Physics |
Online Access: | https://jurnal.uns.ac.id/ijap/article/view/1422 |
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doaj-7ea23529a16b476e9c5f58d7b2ca828d2020-11-24T20:52:28ZengSebelas Maret UniversityIndonesian Journal of Applied Physics2089-01332477-64162017-02-01602798710.13057/ijap.v6i02.14224260STRUCTURE MODELLING OF SUBSURFACE BY USING KIRCHHOFF MIGRATION METHOD AND FINITE DIFFERENCE ANISOTROPY METHODHusni Cahyadi Kurniawan0Adi Susilo1Teguh SurosoBrawijaya UniversityBrawijaya UniversityThe image of subsurface with a migration method keeps on developing to get an image result which the closest in real condition. The conditions in subsurface are very complex and variables it couses the process of wave propagation which can not be judged as the same in every layers. so it is needed an anisotropy pharameter analysiz (η) in seismic data migration process. The research will compare two kinds of migrations those are Kirchhoff migration and finite difference anisotropy. It is done because not all datas are processed by anisotropy, even with isotropi it will get good result. The result of kirchoff migration has not so good quality (low resolution) on the first layer reflector.but on the second and third layer reflector have good result (high resolution). I estimate that in the first layer reflector there is anistropi influence, because the ratio effect between far offset and the depth is hight. The analysis result get η ansotropi pharameter result as 0,25 and put into migration process. On the second migration process is finite difference anisotropy appears on the first layer reflector and shows high resolution and suitable with the real layer model.https://jurnal.uns.ac.id/ijap/article/view/1422 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Husni Cahyadi Kurniawan Adi Susilo Teguh Suroso |
spellingShingle |
Husni Cahyadi Kurniawan Adi Susilo Teguh Suroso STRUCTURE MODELLING OF SUBSURFACE BY USING KIRCHHOFF MIGRATION METHOD AND FINITE DIFFERENCE ANISOTROPY METHOD Indonesian Journal of Applied Physics |
author_facet |
Husni Cahyadi Kurniawan Adi Susilo Teguh Suroso |
author_sort |
Husni Cahyadi Kurniawan |
title |
STRUCTURE MODELLING OF SUBSURFACE BY USING KIRCHHOFF MIGRATION METHOD AND FINITE DIFFERENCE ANISOTROPY METHOD |
title_short |
STRUCTURE MODELLING OF SUBSURFACE BY USING KIRCHHOFF MIGRATION METHOD AND FINITE DIFFERENCE ANISOTROPY METHOD |
title_full |
STRUCTURE MODELLING OF SUBSURFACE BY USING KIRCHHOFF MIGRATION METHOD AND FINITE DIFFERENCE ANISOTROPY METHOD |
title_fullStr |
STRUCTURE MODELLING OF SUBSURFACE BY USING KIRCHHOFF MIGRATION METHOD AND FINITE DIFFERENCE ANISOTROPY METHOD |
title_full_unstemmed |
STRUCTURE MODELLING OF SUBSURFACE BY USING KIRCHHOFF MIGRATION METHOD AND FINITE DIFFERENCE ANISOTROPY METHOD |
title_sort |
structure modelling of subsurface by using kirchhoff migration method and finite difference anisotropy method |
publisher |
Sebelas Maret University |
series |
Indonesian Journal of Applied Physics |
issn |
2089-0133 2477-6416 |
publishDate |
2017-02-01 |
description |
The image of subsurface with a migration method keeps on developing to get an image result which the closest in real condition. The conditions in subsurface are very complex and variables it couses the process of wave propagation which can not be judged as the same in every layers. so it is needed an anisotropy pharameter analysiz (η) in seismic data migration process. The research will compare two kinds of migrations those are Kirchhoff migration and finite difference anisotropy. It is done because not all datas are processed by anisotropy, even with isotropi it will get good result. The result of kirchoff migration has not so good quality (low resolution) on the first layer reflector.but on the second and third layer reflector have good result (high resolution). I estimate that in the first layer reflector there is anistropi influence, because the ratio effect between far offset and the depth is hight. The analysis result get η ansotropi pharameter result as 0,25 and put into migration process. On the second migration process is finite difference anisotropy appears on the first layer reflector and shows high resolution and suitable with the real layer model. |
url |
https://jurnal.uns.ac.id/ijap/article/view/1422 |
work_keys_str_mv |
AT husnicahyadikurniawan structuremodellingofsubsurfacebyusingkirchhoffmigrationmethodandfinitedifferenceanisotropymethod AT adisusilo structuremodellingofsubsurfacebyusingkirchhoffmigrationmethodandfinitedifferenceanisotropymethod AT teguhsuroso structuremodellingofsubsurfacebyusingkirchhoffmigrationmethodandfinitedifferenceanisotropymethod |
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1716799563653709824 |