MAGNETOTELLURIC INVESTIGATIONS ALONG THE URSEIS PROFILE: FIRST RESULTS

dc.contributor.author	Borner R.U.
dc.contributor.author	Oelsner C.
dc.contributor.author	Vygodner K.
dc.date.accessioned	2021-01-11T02:44:29Z
dc.date.available	2021-01-11T02:44:29Z
dc.date.issued	1999
dc.identifier	https://elibrary.ru/item.asp?id=1018714
dc.identifier.citation	International Journal of Earth Sciences, 1999, , 4, 511-514
dc.identifier.issn	1437-3254
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/22580
dc.description.abstract	An interpretation of an E-W profile of 30 magnetotelluric field stations along the URSEIS transect is presented. The magnetotelluric instruments used covered a period range from 0.2 to approximately 500 s and thus enabled a resolution of shallow and upper crustal structures. After decomposition of the impedance tensor a 2D interpretation was performed. The model obtained by a 2D inversion displays a conductive zone west of the Main Uralian Fault. It appears to be consistent with a tectonic division obtained by URSEIS seismic studies.
dc.subject	MAGNETOTELLURIC METHOD
dc.subject	URSEIS
dc.subject	EARTH'S CRUST ELECTRICAL CONDUCTIVITY
dc.subject	2D MODELING
dc.title	MAGNETOTELLURIC INVESTIGATIONS ALONG THE URSEIS PROFILE: FIRST RESULTS
dc.type	Статья

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