Please use this identifier to cite or link to this item: http://ir.futminna.edu.ng:8080/jspui/handle/123456789/19050
Title: Aero-magnetic and Aero-radiometric Prospecting for Potential Gold Mineralisation over Ilesha and its Environs Southwest, Nigeria
Authors: O., K. Akinduko
A., Salako, Kazeem
D., Alhassan, Usman
O., Lawrence, Jane
Alkali, , Aisha
B., Aliyu, Shakirat
Abdullahi, , Muhammad
Adewumi, Taiwo
Damidami, , Luka
Keywords: Aero-magnetic; aero-radiometric; analytic signal; hydrothermal alteration; au mineralization; Nigeria
Issue Date: 21-Dec-2022
Publisher: Asian Journal of Geological Research
Citation: O.K. Akinduko, A. Salako Kazeem, D. Alhassan Usman, Lawrence, J. O., Alkali Aisha, B. Aliyu Shakirat, Abdullahi Muhammad, Adewumi Taiwo & Damidami Luka (2022): Aero-magnetic and Aero-radiometric prospecting for Gold Mineralisation over Ilesha and its Environs Southwest, Nigeria. Asian Journal of Geological Research (AJOGER), 5(4), pp. 1-16.
Series/Report no.: Asian Journal of Geological Research Volume 5, Issue 4, Page 1-16, 2022;no.AJOGER.96016
Abstract: The mapping of potential gold mineralization zones in a part of southwestern Nigeria was carried out from the analyses and interpretation of airborne magnetic and radiometric data. Some enhancing filters, such as analytic signal and first vertical derivative were applied on the Total Magnetic Intensity map to delineate near-surface structures that might host the potential mineral zones within the study area. The analytic signal shows three magnetic zones delineated with low magnetic zone ranging from 0.008 to 0.026 nT/m, moderate with amplitude 0.117 to 0.029 nT/m and high with amplitudes above 0.109 nT/m. In the First vertical derivative, NE-SW structural trends, considered to be the orientation of gold mineral deposits dominate. The depth obtained from the source parameter imaging ranges from 89.03 to 574.76 m. The results from the analysis of aero-radiometric data revealed that the concentration of the radioelements ranged from 0.16 – 3.25 %, 0.80 – 33.27 ppm and 0.13 – 7.24 ppm for potassium, thorium, and uranium, respectively. The K/eTh ratio maps reveal the presence of hydrothermal alteration zones at the north-eastern, central,and southern parts of the study area corresponding to the amphibolite schist and quartz schist, respectively, source rocks for gold deposits. This study has shown that the structures (faults and fractures) and hydrothermal alteration zones delineated within the study area are favourable features to host gold mineralization in the study area.
URI: http://repository.futminna.edu.ng:8080/jspui/handle/123456789/19050
ISSN: E-ISSN: 2321–0990,
P-ISSN: 2321–0982
Appears in Collections:Applied Geophysics

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