A basalt flow and feeding dyke, N.E. Uganda
By: Davies, K.A
.
Material type: 
ArticleDescription: 268-272pp.Subject(s): Basalt flow - Uganda | Dolerite dyke - Loyoro - Karamoja district - Uganda | Volcanic rock - Uganda | Petrology - Uganda
In:
Geological magazine : Vol. 90 Iss. 1-6 Year. 1953Summary: Abstract
Tholeiitic rocks, which are well represented in the igneous history of the African Continent, occur as a dyke and related flow found by the writer in the north-east corner of Uganda. They outcrop in an area which is notable mainly for alkaline intrusions and lavas, so a brief attempt is made to explain the relationships and origins of the rocks in this limited area of the continent.
| Item type | Current location | Collection | Call number | Status | Date due | Barcode |
|---|---|---|---|---|---|---|
Article
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Library and Information Centre Periodical Section | Bound Journal Collection | Not for loan | 002541_44 | ||
Serials/Scientific Journal
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Library and Information Centre Periodical Section | Bound Journal Collection | 550 GEO (Browse shelf) | Available | 002541 |
Abstract
Tholeiitic rocks, which are well represented in the igneous history of the African Continent, occur as a dyke and related flow found by the writer in the north-east corner of Uganda. They outcrop in an area which is notable mainly for alkaline intrusions and lavas, so a brief attempt is made to explain the relationships and origins of the rocks in this limited area of the continent.
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