SEG Technical Program Expanded Abstracts 2014 2014
DOI: 10.1190/segam2014-1323.1
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Using the pseudo-gravity functional transform to enhance deep-magnetic sources and enrich regional gravity data

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Cited by 4 publications
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“…The amplitude of the anomalies is dominated by the magnetic bodies that are present in the shallowest geologic structures. Convectional filtering methods smear out the shallow sources and are not capable of separating the lower amplitude magnetic anomalies associated with the deeper magnetic source rocks [5]. On pseudogravity transformation, [6] explained the significance of employing methods to transform dipole anomalies into monopoles, aiming to enhance the interpretability of the data; [5] explained that 'Poisson's theorem relates linearly the derivative of the gravity taken along the total magnetization distributions.…”
Section: Introductionmentioning
confidence: 99%
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“…The amplitude of the anomalies is dominated by the magnetic bodies that are present in the shallowest geologic structures. Convectional filtering methods smear out the shallow sources and are not capable of separating the lower amplitude magnetic anomalies associated with the deeper magnetic source rocks [5]. On pseudogravity transformation, [6] explained the significance of employing methods to transform dipole anomalies into monopoles, aiming to enhance the interpretability of the data; [5] explained that 'Poisson's theorem relates linearly the derivative of the gravity taken along the total magnetization distributions.…”
Section: Introductionmentioning
confidence: 99%
“…Convectional filtering methods smear out the shallow sources and are not capable of separating the lower amplitude magnetic anomalies associated with the deeper magnetic source rocks [5]. On pseudogravity transformation, [6] explained the significance of employing methods to transform dipole anomalies into monopoles, aiming to enhance the interpretability of the data; [5] explained that 'Poisson's theorem relates linearly the derivative of the gravity taken along the total magnetization distributions. From this theorem, two very useful functional transformations for magnetic anomalies, the reduction-to-pole (RTP) and the pseudogravity (PSG) vertical integration, were formulated by Baranov.'…”
Section: Introductionmentioning
confidence: 99%