INTRINSIC AND LAYER-INDUCED VERTICAL TRANSVERSE ISOTROPY

dc.contributor.authorBakulin A.
dc.date.accessioned2022-02-05T05:13:34Z
dc.date.available2022-02-05T05:13:34Z
dc.date.issued2003
dc.description.abstractAnisotropy 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.identifierhttps://elibrary.ru/item.asp?id=14210694
dc.identifier.citationGeophysics, 2003, 68, 5, 1708-1713
dc.identifier.issn0016-8033
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/34999
dc.titleINTRINSIC AND LAYER-INDUCED VERTICAL TRANSVERSE ISOTROPY
dc.typeСтатья

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