Please use this identifier to cite or link to this item: http://ir.futminna.edu.ng:8080/jspui/handle/123456789/15498
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dc.contributor.authorRafiu, Adewuyi Abdulwaheed-
dc.contributor.authorSalako, Kazeem Adeyinka-
dc.contributor.authorJimoh, Mufutau Owolab-
dc.date.accessioned2022-12-17T15:55:21Z-
dc.date.available2022-12-17T15:55:21Z-
dc.date.issued2022-06-10-
dc.identifier.citation2.Abdulrahaman Idris Augie , Kazeem Adeyinka Salako , Adewuyi Abdulwaheed Rafiu ,Mufutau Owolabi Jimoh (2022).Geophysical assessment for gold mineralization potential over the southern part of Kebbi State using aeromagnetic data Geology, Geophysics and Environment ,vol. 48 (2): 177–193en_US
dc.identifier.issnhttps://doi.org/10.7494/geol.2022.48.2.177 ISSN 2299-8004 | e-ISSN 2353-0790-
dc.identifier.urihttp://repository.futminna.edu.ng:8080/jspui/handle/123456789/15498-
dc.description.abstractThe magnetic signatures over the southern part of Kebbi State and its environs were analyzed together with the geological settings of the area to delineate the structures that may host gold mineralization. The aero magnetic data used was the survey carried out by Fugro airborne surveys between 2005 and 2010 on behalf of the Federal Government of Nigeria. The reduction to equator (RTE), first and second vertical derivatives (FVD and SVD), Centre for Exploration Targeting (CET), analytic signal (AS), source parameter imaging (SPI) and tilt de rivative (TDR) techniques were applied to the magnetic data covering the area. The results of the AS technique revealed that the study area is characterized with high amplitudes of magnetic anomalies (above 0.048 nT/m) and these could be of ferromagnetic minerals such as gold. The FVD, SVD, CET and TDR techniques also helped in delineating the lineaments (such as faults, fractures or shears zones) believed to be associated with alteration zones which play an important role in determining gold mineralized zones. The direction of the orientation of these features/lineaments trended in the NE-SW direction. The faults, fractures or shears zones delineated rep resent veins of possible mineralization. The depth of occurrence to the causative bodies using SPI algorithms was found to be below 137 m. Structures delineated within the area, when compared with the geological setting of the area, correspond to: quartz-mica schist, granite, biotite, gneiss, diorite, medium coarse-grained and biotite horn blende granite. Results from these techniques revealed alteration zones that may host gold. These regions corre spond to the following areas: SE parts of Yauri and Shanga, Fakai, Ngaski, Zuru, Magama, Rijau, and the eastern part of Wasagu/Danko and Bukkuyum.en_US
dc.language.isoenen_US
dc.publisherGeology, Geophysics and Environmenten_US
dc.subjectgold mineralization, Yauri-Zuru schist belt, Centre for Exploration Targeting (CET), first vertical de rivatives (FVD), second vertical derivatives (SVD), source parameter imaging (SPI), tilt derivative (TDR)en_US
dc.titleGeophysical assessment for gold mineralization potential over the southern part of Kebbi State using aeromagneticen_US
dc.title.alternative2.Abdulrahaman Idris Augie , Kazeem Adeyinka Salako , Adewuyi Abdulwaheed Rafiu ,Mufutau Owolabi Jimoh (2022).Geophysical assessment for gold mineralization potential over the southern part of Kebbi State using aeromagnetic data Geology, Geophysics and Environment ,vol. 48 (2): 177–193en_US
dc.typeArticleen_US
Appears in Collections:Applied Geophysics

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