MATHEMATICAL MODELING OF ELASTIC WAVE VELOCITY ANISOTROPY IN A CRACKED GEOLOGICAL MEDIUM

dc.contributor.author	Maslov B.P.
dc.contributor.author	Prodaivoda G.T.
dc.contributor.author	Vyzhva S.A.
dc.date.accessioned	2021-03-02T07:41:51Z
dc.date.available	2021-03-02T07:41:51Z
dc.date.issued	2001
dc.identifier	https://elibrary.ru/item.asp?id=27761601
dc.identifier.citation	Geophysical Journal, 2001, 20, 2, 191-212
dc.identifier.issn	0275-9128
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/26014
dc.description.abstract	A new method has been proposed for the mathematical modeling of the effective elastic constants of a geological medium with arbitrary one, two or three oriented systems of cracks. The method imposes no restrictions as to the concentration or shape of the cracks. Numerical calculations using a "cracked limestone" model have established essential differences between transverse-isotropic and azimuthal-anisotropic velocity of elastic waves with various types of polarisation travelling in "cracked limestone" with different systems of cracks. The established factors can be applied in determining crack systems with seismic methods.
dc.title	MATHEMATICAL MODELING OF ELASTIC WAVE VELOCITY ANISOTROPY IN A CRACKED GEOLOGICAL MEDIUM
dc.type	Статья

Files in this item

Files	Size	Format	View
There are no files associated with this item.