RESULTS OF GEOELECTRIC MEASUREMENTS WITHIN THE OBI COAL DEPOSIT

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dc.contributor.authorAkubue, George Nnabuike
dc.date.accessioned2014-02-07T11:55:18Z
dc.date.available2014-02-07T11:55:18Z
dc.date.issued1977-05
dc.descriptionThesis submitted to the Ahmadu Bello University in partial fulfilment of the requirements for the award of the degree of Master of Scienceen_US
dc.description.abstractResults of Geoelectric measurements within Obi coal deposit show that the host rock which is shale has resistivity ranging from 5 to 14 ohm-m and within the shale exists a sub-section with resistivity from 15 to 30 ohm-m. Correlation with geological data reveals that this section contains the thick coal seams and is of the order of 60m thick generally, Vertical electrical soundings (VES) have marked out the anticlinal structure within the area, and gave indications of three fault zones. Self-potential measurements show one positive and one negative anomalies. While the negative anomaly is interpreted in terms of a fault zone the positive anomaly is attributed to an elevation effect. Gravity measurements show that positive gravity anomalies exist over two fault zones in the area.en_US
dc.identifier.urihttp://hdl.handle.net/123456789/719
dc.language.isoenen_US
dc.subjectRESULTSen_US
dc.subjectGEOELECTRICen_US
dc.subjectMEASUREMENTSen_US
dc.subjectOBIen_US
dc.subjectCOALen_US
dc.subjectDEPOSITen_US
dc.titleRESULTS OF GEOELECTRIC MEASUREMENTS WITHIN THE OBI COAL DEPOSITen_US
dc.typeThesisen_US
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