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Geochronology and metamorphic P-T-X evolution of the Eburnean granulite-facies metapelites of Tidjenouine (Central Hoggar, Algeria): witness of the LATEA metacratonic evolution.

dc.contributor.authorBendaoud, A
dc.contributor.authorOuzegane, K
dc.contributor.authorGodard, G
dc.contributor.authorLiégeois, J.P.
dc.contributor.authorKienast, J.R.
dc.contributor.authorBruguier, O
dc.contributor.authorDrareni, A
dc.contributor.editorENNIH, N. & LIEGEOIS, J.-P.
dc.date2008
dc.date.accessioned2016-03-15T10:02:54Z
dc.date.available2016-03-15T10:02:54Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/29
dc.languageeng
dc.publisherGeological Society
dc.relation.ispartofseriesSpecial Publications
dc.titleGeochronology and metamorphic P-T-X evolution of the Eburnean granulite-facies metapelites of Tidjenouine (Central Hoggar, Algeria): witness of the LATEA metacratonic evolution.
dc.typeBook chapter
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freeGeodynamics and mineral resources
dc.source.titleThe Boundaries of the West African Craton
dc.source.volume297
dc.source.page111-146
Orfeo.peerreviewedYes
dc.identifier.doi10.1144/SP297.6
dc.identifier.url10.1144/SP297.6
dc.identifier.rmca72


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