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11 posed and cance seems poorly where Archean what defined to stretch tectonic signifi- n o r t h of the Zaire craton as far as J e b e l cratonic area Uweinat, and Early P r o t e r o z o i c is r e g a r d e d of rocks as the East Saharan considerable outcrop in the n o r t h e r n part of craton. C. : ~i.. . "" '' .. ' l : E * % I I iI I I aS J I J I I I # i % t I 0ROGEN I C ACTiV[T[ES / I I • ... - . . '. , - ... ~ • ". 3: AFRICAN based KIBARAN BELT UB UBENDIAN BELT CRATON Cratons The b o u n d a r i e s defined K on discontinuities.

The presence of soft sediment folding in the iron-formations suggest gravity displacement in a slope environment. Fig Tree Group Schoongezicht northward south. 8). , characteristics 1988) for have detailed of the Moodies Group lithofacies. been suc- paleoenviron- In the northern Eureka syncline the contact of the Moodies Group with the Fig Tree Group is gradational, poorly sorted, with conglomeratic beds these conglomerates are well ternal grading and weak imbrication, of plane or cross-stratified environments glomeratic modern which sandstones which longitudinal bar facies conglomerates are more Formation, abundant northward dominant in the are while with north.

Vzlw • ,30C~ ~ B~ bertonian JJllSwazilandian ~--J <~m O ~- p ~Belin~ean ! ,n;~,, Gneiss complex (Kaapvaal), Tonalite gneiss (Zimbabwe), Hoggar. Madagascar. 5: Distribution of African orogenies (A); B: Frequency distribution of U-Pb zircon ages from different Precambrian regions. ) 15 It is c o n s i d e r e d relevant here to outline the various arguments that have been advanced in support of some of the above boundaries, for the Proterozoic. Windley (1984) favoured the w o r l d - w i d e A r c h e a n - P r o t e r o z o i c boundary.

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A Trip to the Safari Park

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