Otwarty dostęp

Estimation of Depth to Bouguer Anomaly Sources Using Euler Deconvolution Techniques

Gideon Oluyinka Layade

Gideon Oluyinka Layade

Department of Physics, Federal University of AgricultureAbeokuta,
Wyszukaj tego autora
Sciendo|Google Scholar
Layade, Gideon Oluyinka
, 
Hazeez Edunjobi

Hazeez Edunjobi

Department of Physics, Federal University of AgricultureAbeokuta,
Wyszukaj tego autora
Sciendo|Google Scholar
Edunjobi, Hazeez
, 
Victor Makinde

Victor Makinde

Department of Physics, Federal University of AgricultureAbeokuta,
Wyszukaj tego autora
Sciendo|Google Scholar
Makinde, Victor
 oraz 
Babatunde Bada

Babatunde Bada

Department of Environmental Management & Toxicology, Federal University of AgricultureAbeokuta,
Wyszukaj tego autora
Sciendo|Google Scholar
Bada, Babatunde
  
03 maj 2021
Estimation of Depth to Bouguer Anomaly Sources Using Euler Deconvolution Techniques's Cover Image
O artykule
Poprzedni artykuł
Następny artykuł
Zacytuj
Pobierz okładkę
Kategoria artykułu: Original scientific article
Data publikacji: 03 maj 2021
Zakres stron: 185 - 195
Otrzymano: 18 sty 2021
Przyjęty: 25 sty 2021
DOI: https://doi.org/10.2478/rmzmag-2020-0016
Słowa kluczowe
© 2021 Gideon Oluyinka Layade et al., published by Sciendo
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.

Figure 1

Geological Map of the Study Area.
Geological Map of the Study Area.

Figure 2

Bouguer Gravity Field of Abeokuta.
Bouguer Gravity Field of Abeokuta.

Figure 3

Bouguer Anomaly Map showing some geological features.
Bouguer Anomaly Map showing some geological features.

Figure 4

Radially Averaged Power Spectrum of the Gravity Field.
Radially Averaged Power Spectrum of the Gravity Field.

Figure 5

Residual Anomaly Field (Bouguer Gravity Field High-Pass filtered at 50 km).
Residual Anomaly Field (Bouguer Gravity Field High-Pass filtered at 50 km).

Figure 6

First Horizontal Derivative along X-Direction.
First Horizontal Derivative along X-Direction.

Figure 7

Upward Continued Analytic Signal Map.
Upward Continued Analytic Signal Map.

Figure 8

Euler Solution Map of Abeokuta, for the Structural Index SI = 0.
Euler Solution Map of Abeokuta, for the Structural Index SI = 0.

Figure 9

Euler Solution Map superimpose on the Residual Anomaly Map.
Euler Solution Map superimpose on the Residual Anomaly Map.

Figure 10

Lineament Map of the Study Area, inferred on the Euler Solution Map.
Lineament Map of the Study Area, inferred on the Euler Solution Map.
Język:
Angielski
Częstotliwość wydawania:
4 razy w roku
Dziedziny czasopisma:
Informatyka, Bazy danych i eksploracja danych, Nauki o Ziemi, Geodezja, Geologia i mineralogia, Nauka o materiałach, Charakterystyka i właściwości materiałów
Kanał RSS czasopisma