2015
DOI: 10.1190/geo2014-0544.1
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Review on airborne electromagnetic inverse theory and applications

Abstract: Airborne electromagnetic (AEM) data processing and inversion has progressed from the early conductivity-depth imaging, to 1D inversion for a layered earth model, and most recently to 2D/3D inversions. The new processes have used methods for searching for solutions, applying constraints, and focusing images, such as Occam's, laterally constrained, and holistic inversions. For airborne data imaging and 1D inversion, some algorithms are fast, whereas others have control over data misfit and the vertical or latera… Show more

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Cited by 43 publications
(6 citation statements)
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“…Processed time-domain or frequency-domain AEM data is inverted with the help of 1D, 2D and 3D inversion routines and to calculate the true resistivity or conductivity of the ground [20][21][22].…”
Section: Time Domainmentioning
confidence: 99%
“…Processed time-domain or frequency-domain AEM data is inverted with the help of 1D, 2D and 3D inversion routines and to calculate the true resistivity or conductivity of the ground [20][21][22].…”
Section: Time Domainmentioning
confidence: 99%
“…AEM data interpretation mainly relies on inversion. For a review of various inversion methods for AEM data, refer to Yin et al [5]. AEM inversion methods are mainly divided into deterministic inversion methods based on regularization theory and Bayesian inversion methods based on random sampling [5].…”
Section: Introductionmentioning
confidence: 99%
“…For a review of various inversion methods for AEM data, refer to Yin et al [5]. AEM inversion methods are mainly divided into deterministic inversion methods based on regularization theory and Bayesian inversion methods based on random sampling [5]. Deterministic inversion methods are based on various optimization methods to obtain a single inversion result [6][7], and has been developed to the inversion of 3D model [8][9][10].…”
Section: Introductionmentioning
confidence: 99%
“…Controlled-source electromagnetics (CSEM) has been a well established technology in detecting hydrocarbon bearing formations to do geophysical explorations (Chave and Cox, 1982;Constable et al, 1986). CSEM has been applied to air-bone (Chang-Chun et al, 2015) and cross-well (Alumbaugh and Newman, 1997) geometries, in land (Grayver et al, 2014;Ward and Hohmann, 1988;Zhdanov and Keller, 1994) and/or marine environment (Constable, 2010;Eidesmo et al, 2002;Ellingsrud et al, 2002;MacGregor and Tomlinson, 2014). These applications are based on the high sensitivity of the low-frequency electromagnetic signals to detect high resistivity contrast in the subsurface.…”
Section: Introductionmentioning
confidence: 99%