THE GEOLOGY OF THE DISTRICT AROUND KARUMO, PAIPE AND JIDU IN THE FEDERAL CAPITAL TERRITORY

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dc.contributor.authorALIYU, ALIYU AHMED
dc.date.accessioned2014-02-17T09:03:39Z
dc.date.available2014-02-17T09:03:39Z
dc.date.issued1979
dc.descriptionA THESIS PRESENTED TO THE DEPARTMENT OF GEOLOGY A.B.U. ZARIA.en_US
dc.description.abstractThe area is made up of mig matites, migmatitic gneisses, granite gneisses nnd parphyrablastic granite gneisses, forming part of the migmatitic complex belonging to the Nigerian Precambrian basement complex. These rocks represent various stages of homogenisatinn in the process of migmatisation. They could have been formed by the migmatizotion of the reactivated gneisses and ether supracrustal rocks of the Oaho meyan successions (with ages of about 2,800 - 2,500 million years.)en_US
dc.identifier.urihttp://hdl.handle.net/123456789/1630
dc.language.isoenen_US
dc.subjectGEOLOGY,en_US
dc.subjectDISTRICT,en_US
dc.subjectKARUMO,en_US
dc.subjectPAIPE,en_US
dc.subjectJIDU,en_US
dc.subjectFEDERAL CAPITAL TERRITORYen_US
dc.titleTHE GEOLOGY OF THE DISTRICT AROUND KARUMO, PAIPE AND JIDU IN THE FEDERAL CAPITAL TERRITORYen_US
dc.typeThesisen_US
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