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the transfer of heat, fluids, and gases from the mantle to the crust, crustal deformation and the evolution of sedimentary basins through flexural isostasy in response. However, these large-scale processes
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Dimitri Béchacq. The research will draw on the Martinique HALL 4 demonstration site and its partners: PHEEAC, the Espace Sud Martinique Agglomeration Community, Cerema, BRGM and NBE. The recruited person
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