Geology of the Sabie River Basalt Formation in the Southern Kruger National Park

Koedoe - African Protected Area Conservation and Science

 
 
Field Value
 
Title Geology of the Sabie River Basalt Formation in the Southern Kruger National Park
 
Creator Sweeney, R.J.
 
Subject — Jurassic, igneous, basalt, doleritic, lava, dyke, geochemistry, volcanology, volcano-stratigraphy, Karoo, Lebombo.
Description The Sabie River Basalt Formation (SRBF) in the central Lebombo is a virtually continuous sequence of basaltic lavas some 2 500 m thick that was erupted 200 - 179 Ma ago. Flows are dominantly pahoehoe in character and vary from 2 m to 20 m in thickness. Dolerite dykes cross-cutting the basalt sequence probably represent feeders to this considerable volcanic event. Volcanological features observed within the SRBF are described. Two chemically distinct basaltic magma types are recognised, the simultaneous eruption of which presents an intriguing geochemical problem as to their origins.
 
Publisher AOSIS Publishing
 
Contributor
Date 1986-11-27
 
Type info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion — —
Format application/pdf
Identifier 10.4102/koedoe.v29i1.523
 
Source Koedoe; Vol 29, No 1 (1986); 105-116 2071-0771 0075-6458
 
Language eng
 
Relation
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https://koedoe.co.za/index.php/koedoe/article/view/523/549
 
Coverage — — —
Rights Copyright (c) 1986 R.J. Sweeney https://creativecommons.org/licenses/by/4.0
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