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dc.contributor.authorElem, Joseph Chidiebere-
dc.contributor.authorAnakwuba, Emmanuel K-
dc.date.accessioned2023-04-04T13:38:06Z-
dc.date.available2023-04-04T13:38:06Z-
dc.date.issued2022-05-30-
dc.identifier.citationGLOBAL JOURNAL OF GEOLOGICAL SCIENCES VOL. 20, 2022en_US
dc.identifier.issnISSN 1596-6798-
dc.identifier.uriDOI: https://dx.doi.org/10.4314/gjgs.v20i1.7-
dc.identifier.urihttp://repository.unizik.edu.ng/handle/123456789/505-
dc.descriptionScholary Worken_US
dc.description.abstractThe Asu River Group Shale in the Oshiri area was evaluated using ground magnetic and geoelectrical methods within existing mine. Some exploration programs in the area have resulted to failure due to the fact that project managers have not fully understood the use and importance of geophysics in enhancing the search for mineral deposits. The aim of the study was to delineate the sulphide deposits using ground magnetics and geoelectrical methods. Result of the ground magnetic survey delineated some shallow tectonic structures like fractures and faults which are capable of hosting metallic sulphide deposits. The residual magnetic intensity of the study area indicates very low magnetic field intensities around the central and southern portions of the study area. These low values indicate absence of magnetite in the near surface materials as suggested by previous studies in the area, but could be referred to as zones with shallow tectonic structures which could be faults and/or fractures capable of housing sulphide deposits. The ore bearing veins within the sedimentary rocks have susceptibilities of ≤ -1.8 nT. The low, negative residual susceptibility zone in the southeastern portion of the study area was targeted for the induced polarization IP and electrical resistivity tomography. Four traverses of induced polarization IP and resistivity surveys were carried out with all the profile lines were in the NE-SW direction. Isolated chargeable bodies with values greater than 340msec and a correspondingly low resistivity values (10Ωm-50Ωm), were encountered across some of these profiles. This zone may represent zones with sulphide mineralization. These identified chargeable bodies occur at approximate depth and width range of between 25-30m and 50-70m respectively. The 1D stratigraphic models reveal an average thickness estimate of 11.0m. Using scalar geometric approach, an estimate of 103,513.75tonnes was obtained, representing a relatively economically viable quantity and a worthy target for investors.en_US
dc.language.isoenen_US
dc.publisherGLOBAL JOURNAL OF GEOLOGICAL SCIENCESen_US
dc.subjectGround Magneticsen_US
dc.subjectGeoelectrical Methodsen_US
dc.subjectSulphide depositsen_US
dc.subjectSoutheastern Nigeriaen_US
dc.subjectOshiri Areaen_US
dc.titleAPPLICATION OF GROUND MAGNETICS AND GEOELECTRICAL METHODS IN DELINEATING SULPHIDE DEPOSIT IN OSHIRI AREA, SOUTHEASTERN NIGERIAen_US
dc.typeArticleen_US
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