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dc.contributor.authorBerger, J
dc.contributor.authorCaby, R
dc.contributor.authorLiégeois, J.P.
dc.contributor.authorMercier, J.C.C
dc.contributor.authorDemaiffe, D
dc.date2009
dc.date.accessioned2016-03-15T10:03:26Z
dc.date.available2016-03-15T10:03:26Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/467
dc.descriptionTheAmalaoulaouNeoproterozoic island-arcmassif belongs to theGourmabelt in Mali. The metagabbros and pyroxenites forming the main body of this arc root show the pervasive development of garnet. In the pyroxenites, the latter has grown by reaction between pyroxene and spinel during isobaric cooling. By contrast, in the metagabbros, garnet textures and relations to felsic veins exclude an origin through solid-state reactions only. It is proposed that garnet has grown following dehydration and localized melting of amphibole-bearing gabbros at the base of the arc. The plagioclase-saturated melts represented by anorthositic veins in the metagabbros and by trondhjemites in the upper part of the massif provide evidence for melting in the deep arc crust, which locally generated high-density garnet-clinopyroxene-rutile residues. Garnet growth and melting began around 850 ◦C at 10 kbar and the tonalitic melts were most probably generated around 1050 ◦C at P = 10 kbar. This HT granulitic imprint can be related to arc maturation, leading to a P-T increase in the deep arc root and dehydration and/or dehydration-melting of amphibole-bearing gabbros. Observation of such features in the root of this Neoproterozoic island arc has important consequences, as it provides a link to models concerning the early generation of continental crust.
dc.languageeng
dc.titleDehydration, melting and related garnet growth in the deep root of the Amalaoulaou Neoproterozoic magmatic arc (Gourma, NE Mali)
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freeGeodynamics and mineral resources
dc.source.titleGeological Magazine
dc.source.volume146
dc.source.page173-186
Orfeo.peerreviewedYes
dc.identifier.doi10.1017/S0016756808005499
dc.identifier.rmca87


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