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It contained all of Gondwana except the Congo craton and Atlantica.
The Congo craton came between Proto-Gondwana and Proto-Laurasia about 600 Ma.
The two halves of Rodinia eventually collided with the Congo craton to form the supercontinent Pannotia 600 million years ago.
The Bangweulu Block is a cratonic unit that forms part of the Congo craton of central Africa.
The collision also produced crustal shortening, during which the stratigraphic sequence was tectonically pushed northwards on top of the Congo Craton.
The Damaran-Lufilian-Zambezi Fold Belt separates the Congo craton to the north from the Kalahari.
In Late Neoproterozoic time, the Congo Craton was a low-lying platform the size of the conterminous United States.
By about 500 Ha the Saharan craton was sutured with the Congo craton during the final assembly of Gondwana.
Around 750 million years ago Rodinia rifted apart into three continents: Proto-Laurasia, the Congo craton and Proto-Gondwana.
The geological basement of the central and eastern regions Equatorial Guinea is composed of Precambrian rocks which form a part of the Congo craton.
Iron Ore has also been discovered in the northwestern part of the Archaean Congo Craton (Sangha region), within the Chaillu Block.
Rocks of this age have been found in the Hoggar, in northwest and southwest Nigeria and in Cameroon to the north of the Congo craton.
They resulted from convergence of the Congo Craton to the north with the Kalahari, Bangweulu, Tanzania and West-Nilian cratons to the south.
The cratons are, from south to north, the Kalahari craton, Congo craton, Tanzania craton and West African craton.
It appears to have formed late in the orogeny when the West African craton engaged with the Congo craton, and to have allowed significant dextral strike-slip movement.
The Goiás Ocean, lying to the southwest between the Amazonian craton and the Congo craton, extended into the Pharusian Ocean.
It lies between the Tuareg shield to the west, the Congo craton to the south, the Arabian-Nubian Shield to the east, and the northern African continental margin.
When Rodinia broke up, it split into three pieces: the supercontinent of Proto-Laurasia, the supercontinent of Proto-Gondwana, and the smaller Congo craton.
The Mwembeshi Shear Zone lies between the Congo craton and the Kalahari craton, to the west (in today's orientation) of the Mozambique Belt.
The Congo Craton occupies a large part of central southern Africa, extending from the Kasai region of the DRC into Sudan and Angola.
It is a segment of a broader belt lying between the Congo craton and the Kalahari craton, which also includes the Lufilian Arc and the Damaran belt.
These eclogites and the associated gabbros are interpreted as relics of a fossil subducted slab that marks a suture zone between the Congo Craton to the north and the Kalahari.
These include "Nile Craton", "Sahara Congo Craton", "Eastern Saharan Craton" and "Central Saharan Ghost Craton".
The orthogneisses form part of an extensive region north of the Kalahari craton and east of the Congo Craton that includes large amounts of 1.15-1.0 Ga arc-type rocks containing juvenile crustal components.
The oldest group of sediments in the Katanga supergroup is the Roan, which started to be deposited in a continental rift basin formed after about 880 Ma as the Congo craton pulled away from the Kalahari craton.