Author(s)

George Oduor Otieno¹, John Gitonga Githiri², Willis Jakanyango Ambusso¹

¹Kenyatta University, Nairobi, Kenya.
²Jomo-Kenyatta University of Agriculture, Science and Technology, Nairobi, Kenya.

The geology of Magaoni area is associated with the presence of heavy minerals [1]. Magaoni’s neighbours Maumba and Nguluku where ilmenite was discovered by Tiomin Resource Inc. in 1996, using drilling and chemical analysis [2]. Ilmenite mineral is known to be magnetically weak, but provides observable magnetic response [3]. In this study, ground magnetic survey method was carried out to map magnetic anomalies of established stations, associated with ilmenite bearing formations. The magnetic contour map plotted showed weak and shallow magnetic signatures spread throughout the study area. 2D Euler deconvolution solutions revealed presence of magnetised formations from near surface to a maximum depth of about 450 m at some points. The weak magnetic formations of near surface indicated presence of ilmenite. Energy dispersive X-ray spectroscopy was done on soil samples collected randomly from the study area to determine the percentage of iron and titanium oxides. The results showed elevated values of titanium dioxide, ranging from 1.5% to 13% which is way above the global average of about 0.7% [4]. The percentage of iron oxide was low, ranging from 1.5% to 4%, this being the reason for weak magnetisation of the study area.

Ilmenite, Magnetic Survey, Euler Deconvolution, Spectroscopy

Otieno, G. , Githiri, J. and Ambusso, W. (2016) Integration of Ground Magnetics and Energy Dispersive X-Ray Fluorescence Spectroscopy in Ilmenite Prospection in Magaoni, Kenya. Open Journal of Applied Sciences, 6, 79-88. doi: 10.4236/ojapps.2016.62008.