ANISOTROPIC MIGRATION WEIGHT FOR AMPLITUDE-PRESERVING MIGRATION AND SENSITIVITY ANALYSIS

dc.contributor.authorKiyashchenko D.
dc.contributor.authorKashtan B.
dc.contributor.authorPlessix R.-E.
dc.date.accessioned2022-10-01T05:54:57Z
dc.date.available2022-10-01T05:54:57Z
dc.date.issued2004
dc.description.abstractAn amplitude-preserving anisotropic migration formula is derived in this paper. The migration is viewed as a weighted diffraction stack and the migration weights are estimated with the stationary phase theorem. To obtain a formula easy to implement, the weights are written in terms of quantities computable along the rays. A sensitivity analysis is then carried out to show that, in the vertical transverse isotropic case, the amplitude-preserving migration is mainly governed by two parameters: the anisotropic NMO velocity and the parameter eta. These parameters can be estimated from the data with a velocity (background) analysis. Therefore, it is possible to use this amplitude-preserving anisotropic migration to recover the correct amplitudes versus offset or azimuth in the migrated image.
dc.identifierhttps://elibrary.ru/item.asp?id=13471255
dc.identifier.citationGeophysical Journal International, 2004, 157, 2, 753-763
dc.identifier.issn0956-540X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/38852
dc.subjectanisotropy
dc.subjectmigration weights
dc.subjectray tracing
dc.titleANISOTROPIC MIGRATION WEIGHT FOR AMPLITUDE-PRESERVING MIGRATION AND SENSITIVITY ANALYSIS
dc.typeСтатья

Файлы

Оригинальный пакет

Показано 1 - 1 из 1
Загрузка...
Изображение-миниатюра
Имя:
Kiya_04.pdf
Размер:
260.42 KB
Формат:
Adobe Portable Document Format

Коллекции