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dc.contributor.authorWohlenberg, J.
dc.contributor.authorBhatt, N V
dc.date.accessioned2014-07-10T12:13:24Z
dc.date.available2014-07-10T12:13:24Z
dc.date.issued1972
dc.identifier.citationWohlenberg, J., & Bhatt, N. V. (1972). Report on airmagnetic surveys of two areas in the Kenya rift valley ag. Tectonophysics, 15(1), 143-149.en_US
dc.identifier.urihttp://www.sciencedirect.com/science/article/pii/0040195172900595
dc.identifier.urihttp://hdl.handle.net/11295/72498
dc.description.abstractAirmagnetic surveys have been carried out in two areas within the Kenya Rift system: the Lake Magadi region and the region south of Lake Hannington. In both regions, but particularly in the area south of Lake Hannington, NW-SE trending magnetic anomalies stand out clearly. The source of these anomalies is considered to be in the deeper earth's crust beneath the rift zone. At present no explanation for the anomalies can be offered. There is no convincing evidence from the magnetic data for the occurrence of extended intrusive bodies in the upper part of the earth's crust beneath the rift floor.en_US
dc.language.isoenen_US
dc.publisherUniversity of Nairobien_US
dc.titleReport on airmagnetic surveys of two areas in the Kenya rift valley agen_US
dc.typeArticleen_US
dc.type.materialenen_US


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