Owing to a N–S upfault, with an amplitude of approximately 3 km the sequence of allochthonous sheets is repeated here in two blocks. All of the units and sheets are downfaulted southwestward and located in the same structural order. The ophiolites and greywackes of the major ophiolitic band, which show deformation at the tectonic contact are overlain Upper Riphean terrigenous and carbonate deposits, …
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