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Structural control of Fe-Mn mineralization in Buya-Taka Lafia and their environs, Northwestern Nigeria

dc.contributor.authorNnabo PN3☼, Adekeye JID
dc.contributor.authorBamigboye OS, Adedoyin AD
dc.contributor.authorOwoyemi, OO
dc.date.accessioned2018-10-05T10:38:54Z
dc.date.available2018-10-05T10:38:54Z
dc.date.issued2018
dc.description.abstractThe schist hosted Fe-Mn mineralization in the southernmost part of Zuru schist belt has not been appraised structurally, this work therefore aimed at evaluating the control of these mineralizations. To achieve this aim, the area was mapped geologically; structural data were taking, processed and interpreted. From the Rosset plots of the joints, fault and foliation plane direction, NW and NE directions were conspicuous. These directions were in line with the observed mineralization directions on the geologic map. From the integration of field mapping observation, it is concluded that the brittle structures control the Fe-Mn mineralization in Kaoje and its environs.en_US
dc.description.sponsorshipSelfen_US
dc.identifier.urihttp://hdl.handle.net/123456789/1215
dc.language.isoenen_US
dc.publisherScience Discoveryen_US
dc.subjectMineralizationen_US
dc.subjectStructural Controlen_US
dc.subjectKaojeen_US
dc.subjectManganiteen_US
dc.subjectGoethiteen_US
dc.titleStructural control of Fe-Mn mineralization in Buya-Taka Lafia and their environs, Northwestern Nigeriaen_US
dc.typeArticleen_US

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