EXACT ELASTODYNAMIC GREEN FUNCTIONS FOR SIMPLE TYPES OF ANISOTROPY DERIVED FROM HIGHER-ORDER RAY THEORY

Show simple item record

dc.contributor.author Vavrycuk V.
dc.date.accessioned 2021-03-19T05:26:31Z
dc.date.available 2021-03-19T05:26:31Z
dc.date.issued 2001
dc.identifier https://www.elibrary.ru/item.asp?id=1301119
dc.identifier.citation Studia Geophysica et Geodaetica, 2001, 45, 1, 67-84
dc.identifier.issn 0039-3169
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/26942
dc.description.abstract Using higher-order ray theory, we derived exact elastodynamic Green functions for three simple types of homogeneous anisotropy. The first type displays an orthorhombic symmetry, the other two types display transverse isotropy. In all cases, the slowness surfaces of waves are either ellipsoids, spheroids or spheres. All three Green functions are expressed by a ray series with a finite number of terms. The Green functions can be written in explicit and elementary form similar to the Stokes solution for isotropy. In two Green functions, the higher-order ray approximations form a near-singularity term, which is significant near a kiss singularity. In the third Green function, the higher-order ray approximations also form a near-field term, which is significant near the point source. No effect connected with the line singularity was observed.
dc.title EXACT ELASTODYNAMIC GREEN FUNCTIONS FOR SIMPLE TYPES OF ANISOTROPY DERIVED FROM HIGHER-ORDER RAY THEORY
dc.type Статья


Files in this item

Files Size Format View

There are no files associated with this item.

This item appears in the following Collection(s)

  • ELibrary
    Метаданные публикаций с сайта https://www.elibrary.ru

Show simple item record