Makaha belt

Makaha belt Shamvaian Supergroup Granitoid clast Zim 6 36 482200 8084000 2613 0.2 2a Kober. zircon Hofmann cl aL 2002 ... 

This stacking was diachronous across the era-ton. Deformation was oldest in the western part of the craton (Midlands belt c. 2675 Ma, Horst-wood 1998) intermediate in the north-central part (Harare belt c. 2645 Ma, Wilson et al. 1995 Jelsma et al. 1996 Nesbitt et al. 2000) and youngest in the northeastern part (Dindi-Makaha belts c. 2605Ma, Vinyu et al. 2001 Hofmann et al. 2002). This deformation appears to have culmi nated in an oblique, east-west-directed orogenic event (Fig. 5 Zambezi belt Vinyu et al. 2001). This could be interpreted as the progressive lateral accretion of tectonic domains between 2.68 and 2.60 Ga (Fig. 7). 

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