On the resolution of gravity anomalies
The transformation error of anomalies of the MGGP as a harmonic functions depends on the field’s equipotential surface curvature, anomaly amplitude and the measure of transformation area, reaching according to the kind of trans formation unreasonable values. Gravity anomalies treatment as a harmonic...
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Date: | 2011 |
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Main Author: | |
Format: | Article |
Language: | Ukrainian |
Published: |
Subbotin Institute of Geophysics of the NAS of Ukraine
2011
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Online Access: | https://journals.uran.ua/geofizicheskiy/article/view/117312 |
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Journal Title: | Geofizicheskiy Zhurnal |
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Geofizicheskiy ZhurnalSummary: | The transformation error of anomalies of the MGGP as a harmonic functions depends on the field’s equipotential surface curvature, anomaly amplitude and the measure of transformation area, reaching according to the kind of trans formation unreasonable values. Gravity anomalies treatment as a harmonic functions has poor effectiveness for the deep regional structures. |
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