geophysics-journal-resistivity blogspot.com

Geophysics Journal

Monday, 17 March 2008. Geoelectrical fields in a layered earth with arbitrary anisotropy. In many cases in geoelectrical exploration, the standard model of a layered isotropic half-space is a good approximation to geophysical reality. But sometimes it is useful to extend this model to uniform anisotropic layers. Manuscript received by the Editor September 8, 1997; revised manuscript received July 16, 1998. Of Braunschweig, Inst. of Geophysics and Meterology, Mendelssohn Strasse 3, D-38106. The model of a.

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Geophysics Journal

Interpex offers two software tools that interpret magnetic and gravity profile data. The MAGIX family of software models data in 2, 2. 75 dimensional earth models consisting of bodies and layers whose forward response matches the input data along a single profile line. The magnetic calculations take into account both induced magnetization and possible remanent magnetization. The remanent magnetization is en.

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Geophysics Journal

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Monday, 17 March 2008. Geoelectrical fields in a layered earth with arbitrary anisotropy. In many cases in geoelectrical exploration, the standard model of a layered isotropic half-space is a good approximation to geophysical reality. But sometimes it is useful to extend this model to uniform anisotropic layers. Manuscript received by the Editor September 8, 1997; revised manuscript received July 16, 1998. Of Braunschweig, Inst. of Geophysics and Meterology, Mendelssohn Strasse 3, D-38106. The model of a.

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This web page geophysics-journal-resistivity.blogspot.com states the following, "Geoelectrical fields in a layered earth with arbitrary anisotropy." We saw that the webpage said " In many cases in geoelectrical exploration, the standard model of a layered isotropic half-space is a good approximation to geophysical reality." It also said " But sometimes it is useful to extend this model to uniform anisotropic layers. Manuscript received by the Editor September 8, 1997; revised manuscript received July 16, 1998. of Geophysics and Meterology, Mendelssohn Strasse 3, D-38106."

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