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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.creator Manya, Shukrani
dc.date 2016-03-08T14:13:27Z
dc.date 2016-03-08T14:13:27Z
dc.date 2006
dc.date.accessioned 2018-03-27T08:56:49Z
dc.date.available 2018-03-27T08:56:49Z
dc.identifier 11.1. 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.
dc.identifier http://hdl.handle.net/123456789/697
dc.identifier.uri http://hdl.handle.net/123456789/3987
dc.language en
dc.subject Tanzania Craton
dc.subject Greenstone Belt
dc.subject Crust
dc.subject Mozambique Belt
dc.title Rhyolitic magmas in the Musoma-Mara greenstone belt, Northeast Tanzania: evidence for the presence of an older continental crust in the Tanzania Craton.
dc.type Conference Paper


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