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Geochemical data (major, trace) obtained on the orthogneisses which formed the basement of the Amsaga area (Archean Reguibat Rise, West African Craton) demonstrate: 1) that these gneisses define a calc-alkaline trend of trondhjemitic affinity; 2) the existence of at least two different types of migmatitic orthogneisses in the Amsaga; 3) a perturbation of composition of these orthogneisses during the Archean granulitic event and Proterozoic hydrothermal event (s) which affected the Amsaga.

GEOCHEMISTRY OF THE AMSAGA AREA ORTHOGNEISSES (ARCHEAN REGUIBAT RISE, MAURITANIA)