INTRINSIC AND LAYER-INDUCED VERTICAL TRANSVERSE ISOTROPY
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dc.contributor.author | Bakulin A. | |
dc.date.accessioned | 2022-02-05T05:13:34Z | |
dc.date.available | 2022-02-05T05:13:34Z | |
dc.date.issued | 2003 | |
dc.identifier | https://elibrary.ru/item.asp?id=14210694 | |
dc.identifier.citation | Geophysics, 2003, 68, 5, 1708-1713 | |
dc.identifier.issn | 0016-8033 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/34999 | |
dc.description.abstract | Anisotropy caused by fine layering is often considered responsible for the differences between velocities obtained in sonic-log and seismic experiments. Understanding the link between the two is critical, especially in the current era of most wells being (highly) deviated. | |
dc.title | INTRINSIC AND LAYER-INDUCED VERTICAL TRANSVERSE ISOTROPY | |
dc.type | Статья |
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