Nonlinear LS-RTM based on seismic scale separation and full wavefield multi-parameter FWI

Least-squares migration (LSM) images the subsurface through an inversion process and seeks the reflectivity model that best explains the measured data. This data-fitting process will implicitly compensate for wavefield propagation effects and limited resolution seen with conventional imaging. These...

Full description

Bibliographic Details
Main Authors: Oystein Korsmo, Yang Yang, Nizar Chemingui, Andrey Pankov, Antonio Castiello, Andrew Long
Format: Conference Object
Language:English
Published: Zenodo 2023
Subjects:
Online Access:https://doi.org/10.5281/zenodo.7980546
_version_ 1821667000291688448
author Oystein Korsmo
Yang Yang
Nizar Chemingui
Andrey Pankov
Antonio Castiello
Andrew Long
author_facet Oystein Korsmo
Yang Yang
Nizar Chemingui
Andrey Pankov
Antonio Castiello
Andrew Long
author_sort Oystein Korsmo
collection Zenodo
description Least-squares migration (LSM) images the subsurface through an inversion process and seeks the reflectivity model that best explains the measured data. This data-fitting process will implicitly compensate for wavefield propagation effects and limited resolution seen with conventional imaging. These favourable properties have made it the method of choice in complex geological settings. In this paper, we will discuss the various properties and implementations of LSM and Full Waveform Inversion (FWI) and suggest a new nonlinear least-squares reverse time migration (LS-RTM) implemented in the framework of FWI. The new inversion estimates the earth reflectivity while updating the velocity model at every iteration. We demonstrate the new solution on a field data example from the Norwegian Sea. Open-Access Online Publication: May 29, 2023
format Conference Object
genre Norwegian Sea
genre_facet Norwegian Sea
geographic Norwegian Sea
geographic_facet Norwegian Sea
id ftzenodo:oai:zenodo.org:7980546
institution Open Polar
language English
op_collection_id ftzenodo
op_doi https://doi.org/10.5281/zenodo.798054610.5281/zenodo.7980545
op_relation https://zenodo.org/communities/aseg_extended_abstracts_2023
https://doi.org/10.5281/zenodo.7980545
https://doi.org/10.5281/zenodo.7980546
oai:zenodo.org:7980546
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution Non Commercial No Derivatives 4.0 International
https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode
op_source Australian Society of Exploration Geophysicists Extended Abstracts, Volume 2023, 4th Australasian Exploration Geoscience Conference, Brisbane, 2023, (2023-03-15)
AEGC, Australasian Exploration Geoscience Conference, Brisbane, Australia, 15-17 March 2023
publishDate 2023
publisher Zenodo
record_format openpolar
spelling ftzenodo:oai:zenodo.org:7980546 2025-01-16T23:58:53+00:00 Nonlinear LS-RTM based on seismic scale separation and full wavefield multi-parameter FWI Oystein Korsmo Yang Yang Nizar Chemingui Andrey Pankov Antonio Castiello Andrew Long 2023-03-15 https://doi.org/10.5281/zenodo.7980546 eng eng Zenodo https://zenodo.org/communities/aseg_extended_abstracts_2023 https://doi.org/10.5281/zenodo.7980545 https://doi.org/10.5281/zenodo.7980546 oai:zenodo.org:7980546 info:eu-repo/semantics/openAccess Creative Commons Attribution Non Commercial No Derivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode Australian Society of Exploration Geophysicists Extended Abstracts, Volume 2023, 4th Australasian Exploration Geoscience Conference, Brisbane, 2023, (2023-03-15) AEGC, Australasian Exploration Geoscience Conference, Brisbane, Australia, 15-17 March 2023 FWI RTM Least Squares Migration Multi-Parameter info:eu-repo/semantics/conferencePaper 2023 ftzenodo https://doi.org/10.5281/zenodo.798054610.5281/zenodo.7980545 2024-12-06T08:05:09Z Least-squares migration (LSM) images the subsurface through an inversion process and seeks the reflectivity model that best explains the measured data. This data-fitting process will implicitly compensate for wavefield propagation effects and limited resolution seen with conventional imaging. These favourable properties have made it the method of choice in complex geological settings. In this paper, we will discuss the various properties and implementations of LSM and Full Waveform Inversion (FWI) and suggest a new nonlinear least-squares reverse time migration (LS-RTM) implemented in the framework of FWI. The new inversion estimates the earth reflectivity while updating the velocity model at every iteration. We demonstrate the new solution on a field data example from the Norwegian Sea. Open-Access Online Publication: May 29, 2023 Conference Object Norwegian Sea Zenodo Norwegian Sea
spellingShingle FWI
RTM
Least Squares Migration
Multi-Parameter
Oystein Korsmo
Yang Yang
Nizar Chemingui
Andrey Pankov
Antonio Castiello
Andrew Long
Nonlinear LS-RTM based on seismic scale separation and full wavefield multi-parameter FWI
title Nonlinear LS-RTM based on seismic scale separation and full wavefield multi-parameter FWI
title_full Nonlinear LS-RTM based on seismic scale separation and full wavefield multi-parameter FWI
title_fullStr Nonlinear LS-RTM based on seismic scale separation and full wavefield multi-parameter FWI
title_full_unstemmed Nonlinear LS-RTM based on seismic scale separation and full wavefield multi-parameter FWI
title_short Nonlinear LS-RTM based on seismic scale separation and full wavefield multi-parameter FWI
title_sort nonlinear ls-rtm based on seismic scale separation and full wavefield multi-parameter fwi
topic FWI
RTM
Least Squares Migration
Multi-Parameter
topic_facet FWI
RTM
Least Squares Migration
Multi-Parameter
url https://doi.org/10.5281/zenodo.7980546