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Gold mineralization at Morila is hosted in flat-lying meta-graywacke associated with a Birimian-aged Massigui schist belt in Mali. Three major events of deformation/metamorphism/fluid flow (D 1 , D 2 and D 3 ) are recognized at Morila, with mineralization associated with various increments of deformation and fluid flow during D 2 . Three distinct vein sets V 1 ...
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