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Étude structurale du centre de l'Adrar des Iforas (Mali) : mylonites et tecto...
The Pan-African belt ot the Hoggar and the Adrar des Iforas results from the collision between the West-African Craton and the Pan-African mobile belt. In Mali, the... -
Structural Evolution of the Gold-rich Ashanti Belt, SW Ghana
The Paleoproterozoic Ashanti Belt hosts numerous world class gold deposits such as the Obuasi deposit (60 million ounces) and the Tarkwa deposit (40 million ounces).... -
STRUCTURE OF THE FERKESSEDOUGOU BATHOLITH (SECTOR OF ZUENOULA, CÔTE D'IVOIRE)...
In the West African Craton, the 2.1 Ga period is a major stage of leucogranite production. Because of its localization, its extension as much as its history in the...
