Shield making in Western Kenya

The Precambrian Kisii Series in Western Kenya is unmetamorphosed and contains andesites, rhyolites, quartzites and basalts. The basalts, for which a minimum K-Ar age of 930 My is cited, were sampled at 15 sites, and after A.F. treatment nine sites yielded a stable palaeomagnetic direction which is b...

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Main Author: Onyango, Walter H
Format: Article in Journal/Newspaper
Language:English
Published: 1971
Subjects:
Online Access:http://hdl.handle.net/11295/15867
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spelling ftunivnairobi:oai:http://erepository.uonbi.ac.ke:11295/15867 2023-05-15T18:22:22+02:00 Shield making in Western Kenya Onyango, Walter H 1971 application/pdf http://hdl.handle.net/11295/15867 en eng http://hdl.handle.net/11295/15867 Article 1971 ftunivnairobi 2022-12-28T09:11:01Z The Precambrian Kisii Series in Western Kenya is unmetamorphosed and contains andesites, rhyolites, quartzites and basalts. The basalts, for which a minimum K-Ar age of 930 My is cited, were sampled at 15 sites, and after A.F. treatment nine sites yielded a stable palaeomagnetic direction which is believed to be primary. The mean direction (N= 9) after tilt correction is D= 99°, I=−59°, α= 10°, and the corresponding palaeomagnetic south pole is at 6° N, 12° W with A95= 14°. This pole lies close to several other poles for Africa but it is of a very different age and it cannot be correlated with them. Instead it is suggested that the Kisii pole must form part of a previously undefined polar wander path for the Late Precambrian of Africa proposed in an accompanying paper by Brock and Piper. Article in Journal/Newspaper South pole University of Nairobi Digital Repository South Pole
institution Open Polar
collection University of Nairobi Digital Repository
op_collection_id ftunivnairobi
language English
description The Precambrian Kisii Series in Western Kenya is unmetamorphosed and contains andesites, rhyolites, quartzites and basalts. The basalts, for which a minimum K-Ar age of 930 My is cited, were sampled at 15 sites, and after A.F. treatment nine sites yielded a stable palaeomagnetic direction which is believed to be primary. The mean direction (N= 9) after tilt correction is D= 99°, I=−59°, α= 10°, and the corresponding palaeomagnetic south pole is at 6° N, 12° W with A95= 14°. This pole lies close to several other poles for Africa but it is of a very different age and it cannot be correlated with them. Instead it is suggested that the Kisii pole must form part of a previously undefined polar wander path for the Late Precambrian of Africa proposed in an accompanying paper by Brock and Piper.
format Article in Journal/Newspaper
author Onyango, Walter H
spellingShingle Onyango, Walter H
Shield making in Western Kenya
author_facet Onyango, Walter H
author_sort Onyango, Walter H
title Shield making in Western Kenya
title_short Shield making in Western Kenya
title_full Shield making in Western Kenya
title_fullStr Shield making in Western Kenya
title_full_unstemmed Shield making in Western Kenya
title_sort shield making in western kenya
publishDate 1971
url http://hdl.handle.net/11295/15867
geographic South Pole
geographic_facet South Pole
genre South pole
genre_facet South pole
op_relation http://hdl.handle.net/11295/15867
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