dc.contributor.author | Fentaw, Haile-Michae | |
dc.contributor.author | Gautneb, Håvard | |
dc.contributor.author | Sebhat, Nesibu | |
dc.contributor.author | Mohammed, Seid | |
dc.date.accessioned | 2020-08-26T09:09:22Z | |
dc.date.available | 2020-08-26T09:09:22Z | |
dc.date.issued | 2000 | |
dc.identifier.uri | https://hdl.handle.net/11250/2674224 | |
dc.description.abstract | Precambrian metamorphic rocks of southern Ethiopia, belonging to the Pan-African (Mozambique Belt), host the Moyale graphite deposit. The principal rock units are amphibole schists, quartz-feldspar-mica schists, granodiorites, quartzites and garphite schists. Graphite-bearing units are hoste by quartzites and quartz-feldspar-mica schists and generally form continuous bodies extending for hundreds of meters. A regional variation in grade and flake size of the graphite is noted. From this lateral extent and mode of occurrence, the graphite is believed to be sedimentary in origin. | |
dc.language.iso | eng | |
dc.relation.ispartofseries | NGU Bulletin (436) | |
dc.rights | Navngivelse 4.0 Internasjonal | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | |
dc.subject | GRAFITT | |
dc.subject | OMDANNING | |
dc.subject | PREKAMBRIUM | |
dc.title | The Moyale graphite deposit, Southern Ethiopia | |
dc.type | Journal article | |
dc.description.localcode | 49538 | |
dc.source.pagenumber | 169-173 | |