THE EFFECT OF FLUID SATURATION IN AN ANISOTROPIC MULTI-SCALE EQUANT POROSITY MODEL

dc.contributor.author	Chapman M.
dc.contributor.author	Maultzsch S.
dc.contributor.author	Liu E.
dc.contributor.author	Li X.Y.
dc.date.accessioned	2022-01-29T04:04:27Z
dc.date.available	2022-01-29T04:04:27Z
dc.date.issued	2003
dc.identifier	https://elibrary.ru/item.asp?id=5133334
dc.identifier.citation	Journal of Applied Geophysics, 2003, 54, 3-4, 191-202
dc.identifier.issn	0926-9851
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34675
dc.description.abstract	It is recognised that exchange of fluid between fractures and the rock matrix can have a strong impact on a rock's anisotropic elastic properties. A recent theoretical advance considers the effect of the scale length of the fractures. We show that under certain circumstances, this model can be simplified. The simplified model matches laboratory data. A prediction of the model is that frequency-dependent effects are important for fluid substitution in the anisotropic case.
dc.subject	ANISOTROPIC
dc.subject	SATURATION
dc.subject	EQUANT
dc.title	THE EFFECT OF FLUID SATURATION IN AN ANISOTROPIC MULTI-SCALE EQUANT POROSITY MODEL
dc.type	Статья

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