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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| Datum: | 2016 |
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| Hauptverfasser: | , , |
| Format: | Artikel |
| Sprache: | English |
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Інститут геофізики ім. С.I. Субботіна НАН України
2016
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| Schriftenreihe: | Геофизический журнал |
| Schlagworte: | |
| Online Zugang: | http://dspace.nbuv.gov.ua/handle/123456789/125213 |
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| Назва журналу: | Digital Library of Periodicals of National Academy of Sciences of Ukraine |
| Zitieren: | Predicting Depth of Mineral Deposit using Gravity-Density Downward Correlation by Fourier Transform / E.E. Epuh, J.B. Olaleye, O.G. Omogunloye // Геофизический журнал. — 2016. — Т. 38, № 5. — С. 137-145. — Бібліогр.: 10 назв. — англ. |
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Digital Library of Periodicals of National Academy of Sciences of Ukraine| Zusammenfassung: | 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. The downward continuation depths obtained from the gravity model were compared with that obtained from reflection seismic observation from the study area and the relative error percent were 1.37 % and 0.46 % respectively. |
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