THE RESERVOIR POTENTIALS OF THE BIMA SANDSTONE AROUND WADE HILL, DADINKOWA AND WUYO AREAS OF GOMBE STATE SHEETS (152NE AND 153NW) •

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dc.contributor.authorADINYE TITUSen
dc.creatorADINYE TITUSen
dc.date.accessioned2023-09-22T19:52:34Z
dc.date.available2023-09-22T19:52:34Z
dc.date.issued2010-09-09en
dc.description.abstractThe Bima Sandstone, an entirely continental formation throughout the Upper Benue Trough, is the basal part of the sedimentary succession. The sandstones are interpreted to be of alluvial fan to braided river originen
dc.identifier.urihttps://teras.ng/api/asset/document/65ed6e09-2721-44b0-81ab-299ef713d221en
dc.identifier.urihttps://teras.ng/catalog-item/98b11f57-653b-492c-9e6b-9c29a4acb447en
dc.identifier.urihttp://dspace.teras-network.net:4000/handle/123456789/42841
dc.publisherAbubakar Tafawa Balewa University Bauchien
dc.titleTHE RESERVOIR POTENTIALS OF THE BIMA SANDSTONE AROUND WADE HILL, DADINKOWA AND WUYO AREAS OF GOMBE STATE SHEETS (152NE AND 153NW) •en
dc.typeUndergraduate Thesesen
thesis.degree.levelBachelorsen
thesis.matric.number04/14367/1en
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