THEORY OF DIFFERENTIAL OFFSET CONTINUATION
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
dc.contributor.author | Fomel S. | |
dc.date.accessioned | 2022-02-08T04:40:21Z | |
dc.date.available | 2022-02-08T04:40:21Z | |
dc.date.issued | 2003 | |
dc.identifier | https://elibrary.ru/item.asp?id=31296613 | |
dc.identifier.citation | Geophysics, 2003, 68, 2, 718-732 | |
dc.identifier.issn | 0016-8033 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/35120 | |
dc.description.abstract | I introduce a partial differential equation to describe the process of prestack reflection data transformation in the offset, midpoint, and time coordinates. The equation is proved theoretically to provide correct kinematics and amplitudes on the transformed constant‐offset sections. Solving an initial‐value problem with the proposed equation leads to integral and frequency‐domain offset continuation operators, which reduce to the known forms of dip moveout operators in the case of continuation to zero offset. | |
dc.title | THEORY OF DIFFERENTIAL OFFSET CONTINUATION | |
dc.type | Статья |
Files in this item
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru