2019
DOI: 10.1190/geo2018-0659.1
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A novel semiairborne frequency-domain controlled-source electromagnetic system: Three-dimensional inversion of semiairborne data from the flight experiment over an ancient mining area near Schleiz, Germany

Abstract: We have developed a novel semiairborne frequency-domain electromagnetic (EM) system and successfully tested it within the DESMEX project. The semiairborne approach relies on the fact that part of the system is positioned on the ground and the rest is airborne. This allows us to take advantage of ground and airborne techniques. In particular, a high-moment transmitter can be installed on the earth’s surface, which enables us to inject and induce strong EM fields in the subsurface. Moreover, galvanic coupling is… Show more

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Cited by 31 publications
(16 citation statements)
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“…Due to the moving receivers and the limited 5 s spatial averaging window length, the corresponding data errors derived from the standard deviations of the stacked semi-AEM data were higher than those of the LOTEM measurements. Moreover, the errors decrease with increasing frequency, ranging from 20% to 1% (Smirnova et al, 2019) for 10 Hz to 1000 Hz, respectively. For large offsets (> 2000 m), the signal-to-noise ratio reduced substantially, limiting the depth of investigation.…”
Section: Semi-aem Surveymentioning
confidence: 97%
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“…Due to the moving receivers and the limited 5 s spatial averaging window length, the corresponding data errors derived from the standard deviations of the stacked semi-AEM data were higher than those of the LOTEM measurements. Moreover, the errors decrease with increasing frequency, ranging from 20% to 1% (Smirnova et al, 2019) for 10 Hz to 1000 Hz, respectively. For large offsets (> 2000 m), the signal-to-noise ratio reduced substantially, limiting the depth of investigation.…”
Section: Semi-aem Surveymentioning
confidence: 97%
“…The gaps in data coverage over the vicinities of source positions can be filled in by the data from the other transmitter. The recorded magnetic fields were subsequently processed in the frequency-domain (Smirnova et al, 2019), resulting in CSEM transfer functions (T z ) between the vertical component of the magnetic field and the current. Where ( ) ( ) ( ), ( ) denotes the observed magnetic flux densities and the ( ) indicates the injection currents (Becken et al, 2020).…”
Section: Semi-aem Surveymentioning
confidence: 99%
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