- GeoRef, Copyright 2004, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States
Petrographic study of rock specimens collected across the axis of the Quihita-Cunene gabbro intrusion from Pocolo to Gambos, and to the south near the Cunene river, Angola, indicates that the gabbroic massif is probably a single intrusion differentiated into a series of layered rocks. Rhythmic and cryptic layering are present. Comparison is made with the Great Dyke of Southern Rhodesia.