Possible zircon UPb evidence for Pan-African granulite-facies metamorphism in the Mozambique belt of southern Tanzania
Identifieur interne : 001547 ( Main/Exploration ); précédent : 001546; suivant : 001548Possible zircon UPb evidence for Pan-African granulite-facies metamorphism in the Mozambique belt of southern Tanzania
Auteurs : J. J. M. M. M Coolen [Pays-Bas] ; H. N. A Priem [Pays-Bas] ; E. A. Th Verdurmen [Pays-Bas] ; R. H Verschure [Pays-Bas]Source :
- Precambrian Research [ 0301-9268 ] ; 1982.
Abstract
Four zircon fractions of garnet-bearing two-pyroxene granulite, from the Furua granulite complex of southern Tanzania, plot very close to concordia. A discordia yields a lower intercept at 652 ± 10 Ma, an age slightly higher than the RbSr whole-rock and mineral ages reported from the surrounding amphibolite-facies rocks. The UPb systematics indicate the presence of a very small amount of older (2–3 Ga) radiogenic lead. The zircon data may be interpreted as indicating an event of granulite-facies metamorphism during the Pan-African thermotectonic episode. This interpretation is at variance with current models postulating that the granulite complexes in the Mozambique belt are relicts of older, possibly Archaean events of metamorphism.
Url:
DOI: 10.1016/0301-9268(82)90152-8
Affiliations:
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<front><div type="abstract" xml:lang="en">Four zircon fractions of garnet-bearing two-pyroxene granulite, from the Furua granulite complex of southern Tanzania, plot very close to concordia. A discordia yields a lower intercept at 652 ± 10 Ma, an age slightly higher than the RbSr whole-rock and mineral ages reported from the surrounding amphibolite-facies rocks. The UPb systematics indicate the presence of a very small amount of older (2–3 Ga) radiogenic lead. The zircon data may be interpreted as indicating an event of granulite-facies metamorphism during the Pan-African thermotectonic episode. This interpretation is at variance with current models postulating that the granulite complexes in the Mozambique belt are relicts of older, possibly Archaean events of metamorphism.</div>
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