| dc.contributor.author | Reilly, T. A | |
| dc.contributor.author | Mussett, A. E. | |
| dc.contributor.author | Raja, P. K. S. | |
| dc.contributor.author | Grasty, R. L | |
| dc.contributor.author | Walsh, J. | |
| dc.date.accessioned | 2014-04-01T12:16:17Z | |
| dc.date.available | 2014-04-01T12:16:17Z | |
| dc.date.issued | 1966-06 | |
| dc.identifier.citation | Reilly, T. A., Mussett, A. E., & Raja, P. K. S. (1966). Age and polarity of the Turkana lavas, north-west Kenya. Nature, 210, 1145-1146. | en_US |
| dc.identifier.uri | http://adsabs.harvard.edu/abs/1966Natur.210.1145R | |
| dc.identifier.uri | http://hdl.handle.net/11295/65704 | |
| dc.description.abstract | THE extension of the Trap Series of Ethiopia into north-west Kenya has previously been suggested on stratigraphical and petrological grounds1. This area has recently been mapped on the basis of a reconnaissance2, and the following succession suggested: Rhyolites and andesites Tvr, Tvd Olivine basalts Tvb2 Phonolites and nephelinites Tvp Augite and analcime basalts Tvb1 Turkana grits Tm | en_US |
| dc.language.iso | en | en_US |
| dc.publisher | University of Nairobi | en_US |
| dc.title | Age and Polarity of the Turkana Lavas, North-west Kenya | en_US |
| dc.type | Article | en_US |
