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

The results show that the projected residual gravity anomaly at depth between 2015 m and 2170 m depicts all the gravity features that are clearly associated with that on the original plane and also show minimal distortion of the shape of the anomalies. The anomalous mass lies between these depths. T...

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Bibliographic Details
Main Authors: Epuh, E.E., Olaleye, J.B., Omogunloye, O.G.
Format: Article
Language:English
Published: Інститут геофізики ім. С.I. Субботіна НАН України 2016
Series:Геофизический журнал
Subjects:
Online Access:http://dspace.nbuv.gov.ua/handle/123456789/125213
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