The Moyale graphite deposit, Southern Ethiopia

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

Med mindre annet er angitt, så er denne innførselen lisensiert som Navngivelse 4.0 Internasjonal