1887

Abstract

The characteristics of frequency domain EM system give it a broad frequency range and more than 5 orders of range for resistivity. The smaller size allows a rigid geometry and thereby in-phase data. Resistivity from phase angle is very sensitive across a wide range, and relatively independent of altitude, as well as measuring magnetic susceptibility and dielectric. The smaller size also allows a coaxial (X) component and close terrain following for the best possible lateral resolution. HFEM should be used where near-surface vertical and lateral resolution are essential, and where geology is resistive or targets weakly conductive.

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/content/papers/10.3997/2214-4609-pdb.383.AEM2013_DAY2_SESSION_5A_Hodges
2013-10-10
2024-04-23
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.383.AEM2013_DAY2_SESSION_5A_Hodges
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