The geological evolution of the Magondi Mobile Belt, Zimbabwe
The Zimbabwe Archaean craton is flanked to the NW by the Magondi Mobile Belt. Within this belt, Magondi Supergroup volcanics and sediments were deposited during the early Proterozoic before being deformed and metamorphosed ∼ 1850 Ma ago. ... The cordier- ite-andalusite pair obviously reflects a pretec- tonic high geothermal gradient, possibly ...
WhatsApp: +86 18221755073