Please use this identifier to cite or link to this item: http://repository.futminna.edu.ng:8080/jspui/handle/123456789/12488
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dc.contributor.authorAlhassan, D.U-
dc.contributor.authorSalako, K.A-
dc.contributor.authorJonah, S.A-
dc.date.accessioned2021-08-05T14:23:21Z-
dc.date.available2021-08-05T14:23:21Z-
dc.date.issued2010-11-
dc.identifier.citationAlhassan, D.U., Dagana, L.M, Salako, K.A., Jonah, S.A and Ofor, N.P (2010)en_US
dc.identifier.urihttp://repository.futminna.edu.ng:8080/jspui/handle/123456789/12488-
dc.description.abstractThis paper discussed the seismic refraction survey conducted at the southern part of Niger State college of Education Minna, in which a three- channel seismograph was used for the survey, the profiles were marked at 100m intervals, while the profiles lines traversed 1000m (1 km). The exact site surveyed covers a total area of about 500, 000 m2. From the data collected, time – distance curves for each shot points were drawn, the velocities of the underlying layers for each points were obtained and the depths to the refractor layer were computed. The results obtained gave an overview of the lateral variation in the lithological changes of the subsurface earth materials in the surveyed area. The basement surface varied in the depth, from depths as shallow as 2.05 into a maximum of 10.13 m. The rock material identified in the surveyed area are chiefly sand, saturated clay, gravel and graniteen_US
dc.description.sponsorshipSelfen_US
dc.language.isoenen_US
dc.publisherBAYERO JOURNAL OF PURE AND APPLIED SCIENCES, 3(2) 56-61en_US
dc.relation.ispartofseries;3(2) 56-61-
dc.subjectbasementen_US
dc.subjectaquiferen_US
dc.subjectseismographen_US
dc.subjecttime-distance curveen_US
dc.subjectvelocityen_US
dc.titleSEISMIC REFRACTION INVESTIGATION OF THE SUBSURFACE STRUCTURE AT THE SOUTHERN PART OF NIGER STATE COLLEGE OF EDUCATION, MINNA, NIGERIAen_US
dc.typeArticleen_US
Appears in Collections:Applied Geophysics

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