2018
DOI: 10.1016/j.jappgeo.2018.04.007
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Exploration of buried carbonate aquifers by the inverse and forward modelling of the Controlled Source Audio-Magnetotelluric data

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Cited by 10 publications
(4 citation statements)
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“…As shown in Figure 12, a goaf with accumulated water is detected as an anomaly with a low apparent resistivity. CSAMT can be used to detect the distribution of groundwater and identify the geological structures in coal seams and gas-rich areas [62]. It has a moderate detection depth, and it is suitable for exploring water and mineral resources owing to the strong and high-quality observation signals.…”
Section: Controllable-source Audio Magnetotelluricsmentioning
confidence: 99%
“…As shown in Figure 12, a goaf with accumulated water is detected as an anomaly with a low apparent resistivity. CSAMT can be used to detect the distribution of groundwater and identify the geological structures in coal seams and gas-rich areas [62]. It has a moderate detection depth, and it is suitable for exploring water and mineral resources owing to the strong and high-quality observation signals.…”
Section: Controllable-source Audio Magnetotelluricsmentioning
confidence: 99%
“…In recent years, the Controlled Source Audio Geodetic Electromagnetic Method (CSAMT) has been developing rapidly, and its application in the detection of geological structures [5], geothermal [6] and minerals [7] has achieved remarkable results. In particular, CSAMT is used to detect underground geological structures with the characteristics and advantages of high resolution, high reliability and large detection depth, and it can effectively detect, identify and differentiate stratigraphic structures and fracture structures [8].…”
Section: Introductionmentioning
confidence: 99%
“…In addition, electrical tomography provides a more precise definition of lithological and structural relationships in the explored area. Electromagnetic methods, including the magnetotelluric method, especially controlled-source audio-magnetotellurics (CSAMT) [7] and the transient electromagnetic method (TEM or TDEM), can be also used in such explorations [8,9]. Both methods are also based on rock resistivity measurements, and similar results are expected as with electrical tomography methods, but they have an advantage in greater depth penetrations, those exceeding 100 m. However, their negative side is high sensitivity to electrical noises, which can often be unavoidable in shallow explorations.…”
Section: Introductionmentioning
confidence: 99%