A Basalt Flow and Feeding Dyke, N.E. Uganda
- 1 August 1953
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 90 (4) , 268-272
- https://doi.org/10.1017/s0016756800065456
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.Keywords
This publication has 3 references indexed in Scilit:
- KARROO DOLERITES OF THE UNION OF SOUTH AFRICAGSA Bulletin, 1949
- Ring Structures with Carbonate Cores in Southern RhodesiaGeological Magazine, 1946
- Sur les roches hyperalcalines d'EgypteBulletin de la Société française de Minéralogie, 1936