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Shamvaian Supergroup

Harare bell Shamvaian Supergroup Greywacke ZIM6. 10-13. 20 30... [Pg.184]

Makaha belt Shamvaian Supergroup Granitoid clast Zim 6 36 482200 8084000 2613 0.2 2a Kober. zircon Hofmann cl aL 2002 ... [Pg.187]

Harare bell Shamvaian Supergroup Granitoid clast B9-S-I9 36 351300 8090700 2650 X X Kober. zircon Dougherly-Page 1994 H W n... [Pg.187]

Harare belt Shamvaian Supergroup Granitoid clast 89-S-25 36 351300 8090700 2670 X X Kober. zircon Dougherty-Page 1994 ... [Pg.187]

Chinhoyi belt Shamvaian Supergroup Granitoid clast S9-C-20 + 2S rim 36 204000 6079500 2800 40 2o Kober. zircon Dougherly>Page 1994 Z... [Pg.187]

Harare bell Shamvaian Supergroup Granitoid clast S9-S-I2 36 351300 8090700 2921 20 3a Kober, zircon Dougherty-Page 1994 Tl... [Pg.187]

Clastic sedimentary rocks cap the stratigraphy in most greenstone belts and have been referred to as the Shamvaian Supergroup (Fig. 5). The central part of the Midlands greenstone belt is occupied by a narrow (1-10 km) NNE-trending fault-bounded unit of clastic sedimentary rocks, interbedded with felsic volcanic rocks (Fig. 3e, Bliss 1970 Harrison 1970 Wilson 1979). A similar unit is found in the Harare belt (Fig. 3g). Both... [Pg.201]

See other pages where Shamvaian Supergroup is mentioned: [Pg.199]    [Pg.203]    [Pg.204]    [Pg.199]    [Pg.203]    [Pg.204]   
See also in sourсe #XX -- [ Pg.199 , Pg.201 , Pg.202 ]



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