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HISTORICAL EVOLUTION OF THE GEOLOGICAL RESEARCHES IN THE MENDERES MASSIF

2009
- The Pan-African basement of Menderes Massif is made up of homogenous paragneiss and schistunits (metaclastic sequence) which are intruded by metagabbros and gneisses derived from different types ofgranites. The basement is unconformably overlain by lower Palaeozoic metaclastic series consisting of quartziteand metaconglomerate at the lowest level ...
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