Please use this identifier to cite or link to this item: http://irepo.futminna.edu.ng:8080/jspui/handle/123456789/30353
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dc.contributor.authorAlfa, I.A.-
dc.contributor.authorAdeniyi, J.O.-
dc.contributor.authorUdensi, E.E.-
dc.contributor.authorJonah, S.A.-
dc.date.accessioned2026-03-14T03:16:29Z-
dc.date.available2026-03-14T03:16:29Z-
dc.date.issued2007-
dc.identifier.urihttp://irepo.futminna.edu.ng:8080/jspui/handle/123456789/30353-
dc.description.abstractA refraction survey was conducted over an area of 1⁄2 km x 1⁄2 km at the Ahmadu Bahago Senior Secondary School, Minna, in order to study the nature of the geological features and to determine possible aquifer locations. A total of thirty-six points were shot, and analysis of the recorded data was based on the study of velocity pattern from the time-distance graph obtained from the field data. Usually, high-velocity values correspond to high-density materials at increasing depths. Two layers were identified, the first having velocities ranging from 714.29 ms to 1666.6 ms1 and the second having velocities ranging from 3267.97 ms to 7500 ms. The refractor is situated at a depth ranging from 3.33m to 9.63m. The refractor velocities are likely associated with granite- granodiorite and granite-gneiss rocks.en_US
dc.language.isoenen_US
dc.publisherEnvironment Technology and Science Journalen_US
dc.subjectSeismicen_US
dc.subjectprofileen_US
dc.subjectrefractoren_US
dc.subjectaquiferen_US
dc.subjectoverburdenen_US
dc.titleSeismic Refraction Investigation of the Subsurface Structure at Ahmadu Bahago Senior Secondary School, Minna, Nigeriaen_US
dc.typeArticleen_US
Appears in Collections:Physics

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