A simple method for deriving the uniform field MT responses in auroral zones.

Accession number;02A0508681
Title;A simple method for deriving the uniform field MT responses in auroral zones.
Author; JONES A G (Geological Survey Of Canada, Ontario, Can) SPRATT J (Geological Survey Of Canada, Ontario, Can)
Journal Title;Earth, Planets Space
Journal Code:G0106B
ISSN:1343-8832
VOL.54;NO.5;PAGE.443-450(2002)
Figure&Table&Reference;FIG.12, TBL.1, REF.41
Pub. Country;Japan
Language;English
Abstract;Source field effects in magnetotelluric data acquired at high geomagnetic latitudes can result in erroneous interpretations of Earth conductivity structure deep within the mantle. This paper describes a simple technique most appropriate for a region that is dominantly one-dimensional(1-D) and uses the vertical magnetic field variations for identifying intervals of likely low contamination by non-uniform sources. Times are chosen when the variations stay within prescribed limits defined on the basis of a histogram of the variations for the whole recording interval. An example is given showing application of the method for data from a site under the auroral oval at a time when solar activity was at its lowest for the last solar cycle. A model derived from the responses obtained by processing all available data implies a decrease in resistivity at about 350km to about 100.OMEGA.m. In contrast, the model obtained from low activity interval responses shows a less rapid decrease in resistivity, without a change at around the 410km phase boundary. The responses obtained from all data can be explained by the influence of a source with an average wavelength of 3,000km. (author abst.)