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Enregistrement W2313605457 · doi:10.4043/otc-19877-ms

Subsalt Imaging Using TTI Reverse Time Migration

2009· article· en· W2313605457 sur OpenAlex

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Notice bibliographique

RevueProceedings of Offshore Technology Conference · 2009
Typearticle
Langueen
DomaineEarth and Planetary Sciences
ThématiqueSeismic Imaging and Inversion Techniques
Établissements canadiensnon disponible
Organismes subventionnairesnon disponible
Mots-clésSeismic migrationGeologyComputer scienceSeismology

Résumé

récupéré en direct d'OpenAlex

SS: The Future of Seismic Imaging; Reverse Time Migration and Full Wavefield Inversion - Subsalt Imaging Using TTI Reverse Time Migration Tony Huang; Tony Huang CGGVeritas Search for other works by this author on: This Site Google Scholar Yu Zhang; Yu Zhang CGGVeritas Search for other works by this author on: This Site Google Scholar Houzhu James Zhang; Houzhu James Zhang CGGVeritas Search for other works by this author on: This Site Google Scholar Jerry Young Jerry Young CGGVeritas Search for other works by this author on: This Site Google Scholar Paper presented at the Offshore Technology Conference, Houston, Texas, May 2009. Paper Number: OTC-19877-MS https://doi.org/10.4043/19877-MS Published: May 04 2009 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Get Permissions Search Site Citation Huang, Tony, Zhang, Yu, Zhang, Houzhu James, and Jerry Young. "SS: The Future of Seismic Imaging; Reverse Time Migration and Full Wavefield Inversion - Subsalt Imaging Using TTI Reverse Time Migration." Paper presented at the Offshore Technology Conference, Houston, Texas, May 2009. doi: https://doi.org/10.4043/19877-MS Download citation file: Ris (Zotero) Reference Manager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentAll ProceedingsOffshore Technology ConferenceOTC Offshore Technology Conference Search Advanced Search AbstractThe development of reverse time migration (RTM) and the availability of wide-azimuth data have significantly increased our ability to image subsalt. Much of this potential, however, remains to be developed by seismic imagers.One area for future development is the incorporation of anisotropy in subsalt imaging. Most anisotropic imaging involves vertical transverse isotropy (VTI), while tilted transverse isotropy (TTI) is generally overlooked. Shale that overlies the dipping salt flanks can cause TTI anisotropy issues. This type of geometry is common in the Deepwater Gulf of Mexico, particularly around salt-withdrawal minibasins. Ignoring the tilted symmetry not only causes image blurring and mispositioning of the salt flank, but also degrades and distorts the base of salt and subsalt images.RTM for isotropic and VTI has been routinely used, but the applications of RTM in a 3D heterogeneous TTI medium is still in its infancy. This lag is the result of difficulties in numerical formulations for non-vertical symmetric axes and the subsequent instabilities. The TTI implementation also carries much higher computational costs than those of isotropic and VTI cases. With the demonstration of its benefits and the advances in computing power, the usage of TTI RTM is expected to increase significantly.Initial applications of TTI RTM used narrow-azimuth, towed-streamer data. The lack of azimuthal information limited the ability to derive the velocity and corresponding anisotropic parameters. More accurate TTI parameters were derived and the benefits of TTI imaging were obtained only when two orthogonal narrow-azimuth datasets were processed simultaneously. The advent of wide-azimuth data in the Deepwater Gulf of Mexico further opens the door for TTI imaging. This is because the wide-azimuth data contains more abundant azimuthal information than either narrow-azimuth or multiple narrow-azimuth datasets.Topics related to TTI RTM remain a focus within the seismic imaging community. Improving the derivation of TTI anisotropic parameters from wide-azimuth data and extending full wavefield inversion for TTI media are among the most active areas of study.IntroductionSeismic imagers routinely apply TTI depth imaging technology to image structures that lie beneath dipping, anisotropic overburden in the Canadian Foothill (Vestrum and Vermeulen, 2004), North Sea (Hawkins et al, 2002) and Offshore West Africa (Ball, 1995). Until now, ray-based migration algorithms served as the only choice for TTI imaging, because upgrading ray-based imaging algorithms for TTI is straightforward and incurs minor additional computational cost. Unlike ray-based algorithms, TTI wave-base algorithms are difficult to formulate and their implementations are often unstable and computationally intensive. Unfortunately, ray-based algorithms perform poorly in comparison to wave-based algorithms in imaging structures beneath such complex overburden as the subsalt in the Gulf of Mexico. This impedes the use of TTI imaging for subsalt in the Gulf of Mexico. The lack of appropriate checkshots and offset VSPs that can be used to constraint anisotropic parameters further discourages the utilization of TTI imaging in the Deepwater Gulf of Mexico. Keywords: annual international meeting, migration, algorithm, upstream oil & gas, offshore technology conference, tomography, velocity field, reservoir characterization, tti rtm, subsalt imaging Subjects: Reservoir Characterization, Seismic processing and interpretation This content is only available via PDF. 2009. Offshore Technology Conference You can access this article if you purchase or spend a download.

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Prédiction distillée sur la base complète

Imitation des enseignants

Ni prévalence calibrée, ni vérité terrain. Validation humaine à venir. Apprise à partir de 10 348 étiquettes directes de Codex et de 10 348 étiquettes directes de Gemma. Le mode candidate est l'union des têtes enseignantes seuillées; le consensus est leur intersection. Ces sorties portent le statut machine_predicted_unvalidated et ne sont ni des étiquettes humaines ni des étiquettes directes de modèles de pointe.

score de la tête « metaresearch » (Codex)0,000
score de la tête « metaresearch » (Gemma)0,000
Version: codex-gemma-dda1882f352aStatut de validation: machine_predicted_unvalidated
Catégories candidatesaucune
Catégories consensuellesaucune
DomaineSignal candidat: aucune · Signal consensuel: aucune
Devis d'étudeSignal candidat: Expérimental (laboratoire) · Signal consensuel: aucune
GenreSignal candidat: Empirique · Signal consensuel: Empirique
Score de désaccord entre enseignants0,454
Score d'incertitude au seuil0,618

Scores Codex et Gemma par catégorie

CatégorieCodexGemma
Métarecherche0,0000,000
Méta-épidémiologie (sens strict)0,0000,000
Méta-épidémiologie (sens large)0,0000,000
Bibliométrie0,0000,001
Études des sciences et des technologies0,0000,000
Communication savante0,0000,000
Science ouverte0,0000,000
Intégrité de la recherche0,0000,000
Charge utile insuffisante (le modèle a refusé de juger)0,0000,000

Scores machine (provisoires)

Les deux têtes enseignantes du modèle étudiant, lues sur ce travail. Un score ordonne la base pour la relecture; il n'affirme jamais une catégorie, et le statut de validation accompagne chaque rangée tel quel.

Scores de référence d'un modèle non mature (critères de maturité non atteints, 7 itérations). Un score ordonne; il n'affirme jamais une catégorie.

Tête enseignante Opus0,015
Tête enseignante GPT0,224
Écart entre enseignants0,209 · la distance entre les deux têtes enseignantes sur ce seul travail
Statut de validationscore_only:v0-immature-baseline · tel quel depuis la passe de notation : score_only signifie que le nombre peut ordonner les travaux, et qu'aucune étiquette de catégorie n'en découle