oa Gravity Modeling of the Southern Madagascar Plateau

The morphology and structure of the Madagascar Plateau must be seen in the context of the geological history of the basins surrounding the Plateau. Pangea the super continent formed with the assembly of Eurasia, Europa, America, Gondwana, began to break up in Permian / lower Triassic followed by continental rifting of the south part of the Pangea and the expansion of the adjacent oceanic plate in the middle Jurassic.