Predicting Depth of Mineral Deposit using Gravity-Density Downward Correlation by Fourier Transform

Predicting Depth of Mineral Deposit using Gravity-Density Downward Correlation by Fourier Transform

Residual gravity anomalies are the superposition of effects originating from several interfaces in the subsurface. In downward projection of the anomalies for the determination of the depth of the particular substructure which accounts for the bulk of the residual gravity anomalies on the plane can...

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Datum:	2016
Hauptverfasser:	Epuh, E. E., Olaleye, J. B., Omogunloye, O. G.
Format:	Artikel
Sprache:	English
Veröffentlicht:	Subbotin Institute of Geophysics of the NAS of Ukraine 2016
Schlagworte:	isostatic residual gravity anomaly downward continuation density log attenuation weighting density function
Online Zugang:	https://journals.uran.ua/geofizicheskiy/article/view/107827
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Назва журналу:	Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal

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