Polymetamorphism in the Paleoproterozoic Ubendian Belt, Tanzania

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dc.contributor.authorBoniface, Nelson
dc.contributor.authorSchenk, Volker
dc.date.accessioned2016-04-22T11:32:46Z
dc.date.available2016-04-22T11:32:46Z
dc.date.issued2007
dc.description.abstractThe Paleoproterozoic (ca. 2.0-1.8 Ga) UbendianUsagaran orogens surrounding the SE and SW margins of the Archaean Tanzania craton contain eclogites of MORBlike chemistry which are among the oldest eclogite occurrences exposed in orogenic belts on Earth. Our study of metamorphic events by petrology and U-Pb SHRIMP dating of zircons is aimed to unravel the orogenic history of the Ubendian Belt southwest of the Tanzania Cratonen_US
dc.identifier.citationBoniface, N.E.L.S.O.N. and Schenk, V., 2007. Polymetamorphism in the Paleoproterozoic Ubendian Belt, Tanzania. Geochimica et Cosmochimica Acta, 71(15 Suppl S), p.A107.en_US
dc.identifier.urihttp://hdl.handle.net/123456789/1647
dc.language.isoenen_US
dc.subjectPolymetamorphismen_US
dc.subjectPaleoproterozoicen_US
dc.subjectUbendian Belten_US
dc.subjectTanzaniaen_US
dc.titlePolymetamorphism in the Paleoproterozoic Ubendian Belt, Tanzaniaen_US
dc.typeJournal Article, Peer Revieweden_US
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