Rhyolitic magmas in the Musoma-Mara greenstone belt, Northeast Tanzania: evidence for the presence of an older continental crust in the Tanzania Craton.

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dc.contributor.authorManya, Shukrani
dc.date.accessioned2016-03-08T14:13:27Z
dc.date.available2016-03-08T14:13:27Z
dc.date.issued2006
dc.identifier.citation11.1. Manya, S., 2006. Rhyolitic magmas in the Musoma-Mara greenstone belt, Northeast Tanzania: evidence for the presence of an older continental crust in the Tanzania Craton. 21st Colloquium of African Geology, pp. 206 in Mozambique.en_US
dc.identifier.urihttp://hdl.handle.net/123456789/697
dc.language.isoenen_US
dc.subjectTanzania Cratonen_US
dc.subjectGreenstone Belten_US
dc.subjectCrusten_US
dc.subjectMozambique Belten_US
dc.titleRhyolitic magmas in the Musoma-Mara greenstone belt, Northeast Tanzania: evidence for the presence of an older continental crust in the Tanzania Craton.en_US
dc.typeConference Paperen_US

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