2003
DOI: 10.1071/aseg2003ab041
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Airborne vector magnetics mapping of remanently magnetised banded iron-formations at Rocklea, Western Australia

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Cited by 2 publications
(2 citation statements)
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“…For current purposes, the target is assumed stationary and at a fixed depth, thereby rendering the magnetic signature static. Assuming that the magnetic signature of the target simply adds to the total magnetic intensity of the local region in a linear fashion, 9 anomalies can easily be identified by simply subtracting the magnetometer reading from the local reference map which is stored on the ground station. Magnetic signature of target.…”
Section: B Total Magnetic Intensity Mapsmentioning
confidence: 99%
“…For current purposes, the target is assumed stationary and at a fixed depth, thereby rendering the magnetic signature static. Assuming that the magnetic signature of the target simply adds to the total magnetic intensity of the local region in a linear fashion, 9 anomalies can easily be identified by simply subtracting the magnetometer reading from the local reference map which is stored on the ground station. Magnetic signature of target.…”
Section: B Total Magnetic Intensity Mapsmentioning
confidence: 99%
“…An ideal absolute three-axis vector magnetometer, on the other hand, also allows the calculation of the TMI while offering diverse additional benefits: It provides full vector information, required for the compensation of magn etic sources associated with the aircraft [9] as well as the detection of remanent magnetization [10]. In contrast to the TMI, the magnetic vector components are furthermore true potential fields, allowing for post processing operations like field continuation [11,12] or inversion [13].…”
Section: Introductionmentioning
confidence: 99%