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dc.contributor.authorRaja, P. K. S
dc.contributor.authorReilly, T. A.
dc.contributor.authorMussett, A. E.
dc.date.accessioned2014-03-24T12:27:15Z
dc.date.available2014-03-24T12:27:15Z
dc.date.issued1966-02
dc.identifier.citationP. K. S. Raja T. A. Reilly A. E. Mussett;The paleomagnetism of the Turkana lavas,1966en_US
dc.identifier.urihttp://onlinelibrary.wiley.com/doi/10.1029/JZ071i004p01217/abstract;jsessionid=FB58E628FF988712C34E021FAEC04DD8.f01t03?deniedAccessCustomisedMessage=&userIsAuthenticated=false
dc.identifier.urihttp://hdl.handle.net/11295/65481
dc.description.abstractDirections of magnetizations obtained after cleaning the Miocene lavas from northwest Kenya are presented. The pole position thus obtained, together with similar data from eastern Africa, indicates that no significant change has occurred from late Eocene to recent times. Observed directions suggest that a late Miocene reversed epoch has occurred.en_US
dc.language.isoenen_US
dc.publisherUniversity of Nairobien_US
dc.titleThe paleomagnetism of the Turkana lavasen_US
dc.typeArticleen_US


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