PENENTUAN MODEL KECEPATA UNTUK PRE-STACK DEPTH MIGRATION MENGGUNAKAN METODE FULL WAVEFORM INVERSION (FWI)

Seismic migration is an important step in the seismic data processing workflow to correct reflectors into their actual position. Based on seismic cross section result, seismic migration is divided into two domains namely Time-Migration and Depth-Migration. Conventional depth-migration methods genera...

Full description

Saved in:
Bibliographic Details
Main Author: Ardana, Andriana
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/84800
Tags: Add Tag
No Tags, Be the first to tag this record!
Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:84800
spelling id-itb.:848002024-08-17T12:37:44ZPENENTUAN MODEL KECEPATA UNTUK PRE-STACK DEPTH MIGRATION MENGGUNAKAN METODE FULL WAVEFORM INVERSION (FWI) Ardana, Andriana Indonesia Final Project Full Waveform Inversion, Reverse Time Migration INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/84800 Seismic migration is an important step in the seismic data processing workflow to correct reflectors into their actual position. Based on seismic cross section result, seismic migration is divided into two domains namely Time-Migration and Depth-Migration. Conventional depth-migration methods generally use interval velocity models derived from RMS or stacking velocity using the Dix transformation. This interval velocity model often contains poor velocities resulting inaccurate depth migration results, especially in complex geological models. This study uses velocity model resulting from Full-Waveform Inversion (FWI). FWI can produce high resolution velocity models, that can be used as input for depth migration. In addition, the depth-migration stage can also evaluate the accuracy of the FWI velocity model based on the seismic cross-section result. FWI is a seismic imaging method that reconstructs velocity of the medium by minimizing misfit between observed and simulated seismograms. FWI is carried out in several stages. Firstly, forward modelling of wave propagation using an initial velocity model from a source to a receiver. Secondly, estimating residual waveform by comparing modelled and recorded data. Thirdly, carrying out an iterative process of minimizing residual data by updating the initial model with adjoint state and optimization methods. The FWI method is implemented using the Python programming language. The FWI workflow is applied to the Overthrust synthetic velocity model. This reasearch conduct Reverse Time Migration (RTM) as depth-migration algorithm. The results shows that RTM using input good FWI velocity model is more accurate for imaging complex geological structures than conventional model. Furthermore result show that smooth velocity model input provide more accurate RTM image. text
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description Seismic migration is an important step in the seismic data processing workflow to correct reflectors into their actual position. Based on seismic cross section result, seismic migration is divided into two domains namely Time-Migration and Depth-Migration. Conventional depth-migration methods generally use interval velocity models derived from RMS or stacking velocity using the Dix transformation. This interval velocity model often contains poor velocities resulting inaccurate depth migration results, especially in complex geological models. This study uses velocity model resulting from Full-Waveform Inversion (FWI). FWI can produce high resolution velocity models, that can be used as input for depth migration. In addition, the depth-migration stage can also evaluate the accuracy of the FWI velocity model based on the seismic cross-section result. FWI is a seismic imaging method that reconstructs velocity of the medium by minimizing misfit between observed and simulated seismograms. FWI is carried out in several stages. Firstly, forward modelling of wave propagation using an initial velocity model from a source to a receiver. Secondly, estimating residual waveform by comparing modelled and recorded data. Thirdly, carrying out an iterative process of minimizing residual data by updating the initial model with adjoint state and optimization methods. The FWI method is implemented using the Python programming language. The FWI workflow is applied to the Overthrust synthetic velocity model. This reasearch conduct Reverse Time Migration (RTM) as depth-migration algorithm. The results shows that RTM using input good FWI velocity model is more accurate for imaging complex geological structures than conventional model. Furthermore result show that smooth velocity model input provide more accurate RTM image.
format Final Project
author Ardana, Andriana
spellingShingle Ardana, Andriana
PENENTUAN MODEL KECEPATA UNTUK PRE-STACK DEPTH MIGRATION MENGGUNAKAN METODE FULL WAVEFORM INVERSION (FWI)
author_facet Ardana, Andriana
author_sort Ardana, Andriana
title PENENTUAN MODEL KECEPATA UNTUK PRE-STACK DEPTH MIGRATION MENGGUNAKAN METODE FULL WAVEFORM INVERSION (FWI)
title_short PENENTUAN MODEL KECEPATA UNTUK PRE-STACK DEPTH MIGRATION MENGGUNAKAN METODE FULL WAVEFORM INVERSION (FWI)
title_full PENENTUAN MODEL KECEPATA UNTUK PRE-STACK DEPTH MIGRATION MENGGUNAKAN METODE FULL WAVEFORM INVERSION (FWI)
title_fullStr PENENTUAN MODEL KECEPATA UNTUK PRE-STACK DEPTH MIGRATION MENGGUNAKAN METODE FULL WAVEFORM INVERSION (FWI)
title_full_unstemmed PENENTUAN MODEL KECEPATA UNTUK PRE-STACK DEPTH MIGRATION MENGGUNAKAN METODE FULL WAVEFORM INVERSION (FWI)
title_sort penentuan model kecepata untuk pre-stack depth migration menggunakan metode full waveform inversion (fwi)
url https://digilib.itb.ac.id/gdl/view/84800
_version_ 1822010500927455232