Author:
Barton J.M.,Bristow J.W.,Venter F.J.
Abstract
Precambrian granitoid rocks underlie approximately 60 percent of the Kruger National Park. They occur primarily in the western portion of the park and comprise a wide variety of rock including granites, granodiorites, tonalites, trondhjemites and syenites spanning more than 1 500 Ma from the Archaean to the Proterozoic. Remnants of old greenstone belts are also found.
Subject
Ecology,Ecology, Evolution, Behavior and Systematics
Cited by
19 articles.
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