ELECTROMAGNETIC TOMOGRAPHY

dc.contributor.author	Zhdanov M.S.
dc.date.accessioned	2020-04-16T07:05:04Z
dc.date.available	2020-04-16T07:05:04Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=31019927
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 301, 4, 37-41
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16841
dc.description.abstract	The paper discusses a technique for successive visualization of the geoelectric section along vertical planes intersecting the three-dimensional geological medium. An image of the medium is obtained by successively scanning downward along specified vertical planes and combining the images of individual vertical layers into a single three-dimensional model of the medium. The problem of electromagnetic tomography consists of constructing a series of images of vertical sections through the medium that reflect the specific resistivities of the layers and the forms of the boundaries separating them. This paper formulates the main principles of electromagnetic tomography.
dc.title	ELECTROMAGNETIC TOMOGRAPHY
dc.type	Статья

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