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A 3.5 Ga granite–gneiss basement in Guinea: further evidence for early archean accretion within the West African Craton

Identifieur interne : 00BA76 ( Main/Exploration ); précédent : 00BA75; suivant : 00BA77

A 3.5 Ga granite–gneiss basement in Guinea: further evidence for early archean accretion within the West African Craton

Auteurs : Denis Thiéblemont [France] ; Claude Delor [France] ; Alain Cocherie [France] ; Jean Michel Lafon [Brésil] ; Jean Christian Goujou [France] ; Alhassane Baldé [Guinée] ; Mamadou Bah [Guinée] ; Hadi Sané [Guinée] ; C. Mark Fanning [Australie]

Source :

RBID : ISTEX:AF99E6B00935A05AA1C76A69AEC5CDDC4F97B5CB

Descripteurs français

English descriptors

Abstract

Abstract: A granite–gneiss formation (Guélémata Orthogneiss) was mapped on the northern and western slopes of the Mount Nimba hill range in Guinea. The original rocks were high-Al, low-Yb, medium to high-K granites similar to most Archean TTG. Analyses of U and Pb isotopes in zircons, using an ion-microprobe (SHRIMP), gave ages of 3542 and 3535 Ma respectively for the granite–gneiss and a neighbouring granulitic metagabbro. These are the oldest ages so far reported from the Archean Kenema-Man domain of West Africa. Partial melting of an unfractionated basalt under eclogite facies conditions appears to be a suitable model for the origin of the granite–gneiss.

Url:
DOI: 10.1016/S0301-9268(00)00160-1


Affiliations:


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Le document en format XML

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<div type="abstract" xml:lang="en">Abstract: A granite–gneiss formation (Guélémata Orthogneiss) was mapped on the northern and western slopes of the Mount Nimba hill range in Guinea. The original rocks were high-Al, low-Yb, medium to high-K granites similar to most Archean TTG. Analyses of U and Pb isotopes in zircons, using an ion-microprobe (SHRIMP), gave ages of 3542 and 3535 Ma respectively for the granite–gneiss and a neighbouring granulitic metagabbro. These are the oldest ages so far reported from the Archean Kenema-Man domain of West Africa. Partial melting of an unfractionated basalt under eclogite facies conditions appears to be a suitable model for the origin of the granite–gneiss.</div>
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